Researcher Database
Last Updated :2024/07/25
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Profile and Settings
Affiliation
Degree
Profile and Settings
Name (Japanese)
KitanoName (Kana)
IppeiName
202101001925444464
Affiliation
Achievement
Research Interests
Research Areas
Research Experience
- 2022/03 - Today Hokkaido University The Hokkaido University Museum Assistant professor
- 2021/04 - 2022/03 栃木県立博物館 学芸部自然課 学芸企画推進員
- 2019/04 - 2021/03 Kyushu University Faculty of Social and Cultural Studies
- 2018/11 - 2019/03 Kyushu University Faculty of Social and Cultural Studies
- 2018/04 - 2018/10 Kyushu University Faculty of Social and Cultural Studies
Education
- 2014/04 - 2018/03 Kyushu University
- 2012/04 - 2014/03 Kyushu University Graduate School of Social and Cultural Studies
- 2008/04 - 2012/03 Kyushu University School of Sciences Department of Earth and Planetary Sciences
Awards
- 2022/10 第8回北大部局横断シンポジウム実行委員会 第8回北大部局横断シンポジウムベストポスター賞
- 2018/09 日本鉱物科学会 平成２９年度日本鉱物科学会論文賞
受賞者: 小山内康人;中野伸彦;足立達朗;北野一平 - 2018/09 日本鉱物科学会 平成２９年度第５回JMPS学生受賞論文賞
受賞者: 北野一平 - 2016/05 日本地球惑星科学連合 日本地球惑星科学連合２０１６年大会 固体地球科学セッション学生優秀発表賞
受賞者: 北野一平
Published Papers
- Mami TAKEHARA, Kenji HORIE, Tomokazu HOKADA, Sotaro BABA, Atsushi KAMEI, Ippei KITANOJournal of Mineralogical and Petrological Sciences 118 (ANTARCTICA) n/a - n/a 1345-6296 2023 [Refereed]
- Ippei KITANO, Tomokazu HOKADA, Sotaro BABA, Atsushi KAMEI, Yoichi MOTOYOSHI, Prayath NANTASIN, Nugroho I. SETIAWAN, Davaa-ochir DASHBAATAR, Tsuyoshi TOYOSHIMA, Masahiro ISHIKAWA, Takuma KATORI, Nobuhiko NAKANO, Yasuhito OSANAIJournal of Mineralogical and Petrological Sciences 118 (ANTARCTICA) n/a - n/a 1345-6296 2023 [Refereed]
- Sotaro BABA, Prayath NANTASIN, Atsushi KAMEI, Ippei KITANO, Yoichi MOTOYOSHI, Nugroho I. SETIAWAN, Davaa-ochir DASHBAATAR, Tomokazu HOKADAJournal of Mineralogical and Petrological Sciences 118 (ANTARCTICA) n/a - n/a 1345-6296 2023 [Refereed]
- Ippei KITANO, Yasuhito OSANAI, Nobuhiko NAKANO, Ryosuke KATO, Vuong BUI THI SINHJournal of Mineralogical and Petrological Sciences 118 (1) n/a - n/a 1345-6296 2023/01 [Refereed]
- Vuong Bui Thi Sinh, Yasuhito Osanai, Nobuhiko Nakano, Ippei Kitano, Tatsuro Adachi, Anh Tran Tuan, Binh PhamJournal of Asian Earth Sciences 226 105070 - 105070 1367-9120 2022/04 [Refereed]
- Sotaro Baba, Kenji Horie, Tomokazu Hokada, Mami Takehara, Atsushi Kamei, Ippei Kitano, Yoichi Motoyoshi, Prayath Nantasin, Nugroho I. Setiawan, Davaa-ochir DashbaatarGondwana Research 105 243 - 261 1342-937X 2021/09 [Refereed]
- Sotaro Baba, Tomokazu Hokada, Atsushi Kamei, Ippei Kitano, Yoichi Motoyoshi, Prayath Nantasin, Nugroho Imam Setiawan, Davaa-Ochir DashbaatarAntarctic Science 33 (1) 52 - 72 0954-1020 2021/02 [Refereed]
Abstract We describe a major shear zone exposed at Akebono Rock and discuss its deformation and metamorphic history, with a view to providing a better understanding of the geological history of the Lützow-Holm Complex. Three deformation episodes are recognized: D1 produced open folds (F1), boudinage and a regional ductile foliation, whilst the related metamorphic facies is characterized by stable garnet. F1 folding is dominantly preserved in the eastern part of the study area. During D2, an isoclinal to tight asymmetric F2 folds developed mainly in the west part of the region, accompanied by an S2 shear, under biotite facies retrograde metamorphism. The D3 episode involved the formation of the major shear zone, characterized by mylonite and L-tectonite fabrics, which took place at ~610–660°C and 4–5 kbar. Large, sigmoidal garnet core domains have S-shaped inclusion trails, suggesting that syntectonic garnet growth occurred before the formation of the shear zone. EstimatedP-T conditions suggest that the sigmoidal garnet-bearing amphibolite was recrystallized at a deeper crustal level and was brought to a higher level during the formation of the shear zone. Crustal-scale deformation involving syntectonic recrystallization and shearing of Akebono Rock is a key issue for reconsidering the evolution of the Lützow-Holm Complex. - Yasuhito Osanai, Ippei Kitano, Nobuhiko Nakano, Tatsuro Adachi, Kazuhiro Yonemura, Aya Yoshimoto, Yukari Miyashita, Satoshi Komemushi, Masayuki KomatsuThe Journal of the Geological Society of Japan 127 (1) 1 - 24 0016-7630 2021/01/15 [Refereed]
- Dolzodmaa BOLDBAATAR, Yasuhito OSANAI, Nobuhiko NAKANO, Tatsuro ADACHI, Jargalan SEREENEN, Ippei KITANO, Kundyz SYERYEKKHAANJournal of Mineralogical and Petrological Sciences 116 (6) 293 - 308 1345-6296 2021 [Refereed]
- Nguyen Van Thinh, Yasuhito Osanai, Tatsuro Adachi, Bui Thi Sinh Vuong, Ippei Kitano, Nguyen Thuy Chung, Phong K. ThaiChemosphere 263 127912 - 127912 0045-6535 2021/01 [Refereed]
- Masaaki Owada, Yasuhito Osanai, Nobuhiko Nakano, Ippei Kitano, Tatsuro Adachi, Pham Binh, Tran Van TriJournal of Asian Earth Sciences 200 104077 - 104077 1367-9120 2020/09 [Refereed]
- Vuong Thi Sinh Bui, Yasuhito Osanai, Nobuhiko Nakano, Tatsuro Adachi, Ippei Kitano, Masaaki OwadaJournal of Asian Earth Sciences 187 104084 - 104084 1367-9120 2020/01 [Refereed]
- In-situ U–Pb isotope and REE analyses for zircons from ultrahigh temperature metamorphic rocks in the Kannak Complex, Kontum Massif, VietnamVuong Thi Sinh Bui, Yasuhito Osanai, Nobuhiko Nakano, Tatsuro Adachi, Ippei KitanoBulletin of the Graduate School of Integrated Sciences for Global Society, Kyushu University 26 (2) 1 - 9 2019/12 [Refereed]
- Vuong Bui Thi Sinh, Yasuhito Osanai, Christoph Lenz, Nobuhiko Nakano, Tatsuro Adachi, Elena Belousova, Ippei KitanoMinerals 9 (2) 89 - 89 2019/02/01 [Refereed]
Gem-quality zircon megacrysts occur in placer deposits in the Central Highlands, Vietnam, and have euhedral to anhedral crystal shapes with dimensions of ~3 cm in length. These zircons have primary inclusions of calcite, olivine, and corundum. Secondary quartz, baddeleyite, hematite, and CO2 fluid inclusions were found in close proximity to cracks and tubular channels. LA-ICP-MS U-Pb ages of analyzed zircon samples yielded two age populations of ca. 1.0 Ma and ca. 6.5 Ma, that were consistent with the ages of alkali basalt eruptions in the Central Highlands at Buon Ma Thuot (5.80–1.67 Ma), Pleiku (4.30–0.80 Ma), and Xuan Loc (0.83–0.44 Ma). The zircon geochemical signatures and primary inclusions suggested a genesis from carbonatite-dominant melts as a result of partial melting of a metasomatized lithospheric mantle source, but not from the host alkali basalt. Chondrite-normalized rare earth element patterns showed a pronounced positive Ce, but negligible Eu anomalies. Detailed hyperspectral Dy3+ photoluminescence images of zircon megacrysts revealed resorption and re-growth processes. - Vuong BUI THI SINH, Yasuhito OSANAI, Nobuhiko NAKANO, Tatsuro ADACHI, Ippei KITANOJournal of Mineralogical and Petrological Sciences 114 (2) 47 - 59 1345-6296 2019 [Refereed]
- Ippei Kitano, Yasuhito Osanai, Nobuhiko Nakano, Tatsuro Adachi, Ian C.W. FitzsimonsJournal of Asian Earth Sciences 156 122 - 144 1367-9120 2018/05 [Refereed]
- Tomokazu Hokada, Sotaro Baba, Atsushi Kamei, Ippei Kitano, Yoichi Motoyoshi, Prayath Nantasin, Nugroho Imam Setiawan, Davaa-Ochir DashbaatarAntarctic Record 国立極地研究所 61 11 - 56 2432-079x 2017/09 [Refereed]
第58次日本南極地域観測隊（JARE-58）では，2016−2017の夏期期間にリュツォ・ホルム湾，プリンスオラフ海岸，及び，エンダビーランドにおいて地質調査をおこなった．調査隊のメンバーは，日本人地質研究者4名とアジア地域（タイ，インドネシア，モンゴル）の交換科学者3名で構成され，本吉隊長が一部期間の調査に加わった．第58次夏期観測では，「しらせ」搭載の2機の大型ヘリコプター（CH101）とともに観測隊チャーターの小型ヘリコプター（AS350）1機による野外調査の支援がなされた．本稿では，観測計画を実施するための，主に設営面での計画，準備，そして行動経過について報告する．The 58th Japanese Antarctic Research Expedition (JARE-58) conducted geological field surveys in the regions of Lützow-Holm Bay, Prince Olav Coast, and Enderby Land during the 2016−2017 austral summer season. The field party consisted of four Japanese geologists and three Asian geologists (Thai, Indonesian, Mongolian), and was joined periodically by JARE-58 expedition leader, Prof. Motoyoshi. Field parties were supported throughout the summer season by a smaller secondary helicopter (AS350) in addition to two main helicopters (CH101) stationed on the icebreaker Shirase. This report summarizes field preparations and the geological work undertaken, and highlights several key points for future planning and research. - Ippei KITANO, Yasuhito OSANAI, Nobuhiko NAKANO, Tatsuro ADACHIJournal of Mineralogical and Petrological Sciences 日本鉱物科学会 111 (2) 118 - 128 1345-6296 2016 [Refereed]
The Sør Rondane Mountains in East Antarctica consist of the various metamorphic rocks and several plutonic rocks, which are related to formation of Gondwana supercontinent. In order to understand the detrital provenances, LA–ICP–MS zircon U–Pb dating were conducted from metamorphosed sedimentary rocks in southern Sør Rondane Mountains. Detrital cores with ~ 990–730 Ma ages were recognized from zircons in the pelitic gneisses and calc–silicate rocks from Menipa, Imingfjella, Mefjell and Arden, while the pelitic gneiss from Tvihøgda exhibited the Archean to Mesoproterozoic ages of ~ 2630–1060 Ma. The Neoproterozoic zircon ages are recognized not only from metamorphosed sedimentary rocks but also from metamorphosed igneous rocks distributed in the central and southern parts of the mountains. However, the Archean to Mesoproterozoic zircon ages are rare in these areas. The results imply the detrital zircons with the Neoproterozoic ages were probably derived from neighbouring igneous rocks (present metamorphosed igneous rocks), while those with Archean to Mesoproterozoic ages have clearly different provenances because of the lack in the Neoproterozoic components. This study suggests the possibility that southern Sør Rondane Mountains can be considered to be juvenile late Mesoproterozoic to Neoproterozoic terrane partly mixed with the Archean to Mesoproterozoic components. - Yasuhito OSANAI, Krishnan SAJEEV, Nobuhiko NAKANO, Ippei KITANO, Wilbert K.V. KEHELPANNALA, Ryosuke KATO, Tatsuro ADACHI, Sanjeewa P.K. MALAVIARACHCHIJournal of Mineralogical and Petrological Sciences 一般社団法人 日本鉱物科学会 111 (3) 157 - 169 1345-6296 2016 [Refereed]
The regional ultrahigh–temperature (UHT) metamorphism of the Highland Complex, Sri Lanka is well established and has an important role in our understanding of the tectonic history of the Gondwana supercontinent. U–Pb zircon dating of sapphirine–bearing Mg–Al granulites yielded two major metamorphic age populations at approximately 620–590 and 563–525 Ma with no evidence of older zircon cores. Pelitic granulite samples with a Grt–Sil–Spl–Crd assemblage have similar metamorphic ages with concordant data clusters at ~ 602, 563, and 526 Ma and inherited zircon cores aged from 2040 to 1600 Ma. The pelitic granulites also underwent two stages of metamorphism (565–520 and 622–580 Ma). Some of these pelitic granulite samples have inherited zircon cores ranging from 3060 to 760 Ma. Zircons in mafic granulite samples have age ranges of 566–533 and 620–578 Ma. A calc–silicate granulite sample also has similar age populations at 591, 541, and 524 Ma. Combining these new results with previously published ages from Sri Lanka and formerly adjacent continental fragments of Gondwana, we propose that the terranes in southern Madagascar (south of Ranotsara Shear Zone), Northern and Southern Madurai and the Trivandrum Blocks of southern India, the Highland Complex of Sri Lanka, and the Skallen Group in the Lützow–Holm Complex of East Antarctica represent a unique metamorphic belt that regionally experienced the Ediacaran–Cambrian UHT event during the amalgamation of the Gondwana supercontinent.
- Yasuhito OSANAI, Krishnan SAJEEV, Nobuhiko NAKANO, Ippei KITANO, Wilbert K.V. KEHELPANNALA, Ryosuke KATO, Tatsuro ADACHI, Sanjeewa P.K. MALAVIARACHCHIJournal of Mineralogical and Petrological Sciences 一般社団法人 日本鉱物科学会 111 (3) 145 - 156 1345-6296 2016 [Refereed]
The ultrahigh–temperature (UHT) regional metamorphism of Sri Lanka has a significant role in understanding the tectonics and formation of the Gondwana supercontinent. Sri Lanka is specifically important because of its central position in Gondwana, located between southern India, Madagascar and eastern Antarctica. In particular, the Highland Complex has been the focus of several previous studies because of the prominence of metasedimentary rocks that experienced UHT metamorphism. The central Highland Complex of Sri Lanka consists of Spr–bearing Mg–Al rich granulites intercalated with other pelitic, mafic granulites and calc–silicates, which preserve several textural evidences for UHT metamorphism. The calculated peak metamorphic conditions for the Mg–Al rich granulite yielded a temperature range from 910 to 1005 °C at 1.0 GPa, and the pressure varies between 0.9 to 1.2 GPa. The estimated metamorphic P–T conditions and evolution path is in good agreement with previous studies and also to that of similar rock–types from southern Madagascar, southern India and East Antarctica.
- Late Permian plume–related magmatism and tectonothermal events in the Kontum Massif, central VietnamMasaaki OWADA, Yasuhito OSANAI, Nobuhiko NAKANO, Tatsuro ADACHI, Ippei KITANO, Tran Van TRI, Hiroo KAGAMIJournal of Mineralogical and Petrological Sciences 一般社団法人 日本鉱物科学会 111 (3) 181 - 195 1345-6296 2016 [Refereed]
The Kontum Massif is situated in the southern part of Trans Vietnam Orogenic Belt (TVOB), central Vietnam, and contains various types of magmatic and metamorphic rocks, the latter including both ultrahigh–pressure and ultrahigh–temperature units. While geochronological data indicate the existence of two main tectonothermal events at 480–420 Ma and 270–240 Ma, the most intense metamorphic and magmatic activity occurred between the Late Permian and Early Triassic due to continental collision between the South China and Indochina cratons. In this study, U–Pb LA–ICP–MS geochronological analyses of zircon obtained from two samples of metagabbro and one sample of charnockite from the massif yielded a magmatic age range of 260–250 Ma for all three samples and an inherited age of ~ 1400 Ma for the charnockite. These magmatic ages overlap with those documented for peak metamorphism in the Kontum Massif. When combined with Nd isotopic data for granitic rocks and pelitic gneisses from the region, these data suggest that the massif may have been derived from reworked continental crust. Geochemical characteristics of metagabbros from the massif reveal that the parental basaltic magma can be correlated with the Song Da igneous suite situated in the northern part of the TVOB, and was assimilated by crustal materials. The Song Da igneous suite is a member of the Emeishan large igneous province and resulted from Late Permian mantle plume activity. We conclude that the plume–related magma intruded into the deeper part of Kontum Massif and induced ultrahigh–temperature metamorphism of the lower crust by acting as a heat source.
- 北野一平, 小山内康人, 中野伸彦, 足立達朗, 吉本紋九州大学大学院比較社会文化学府紀要「比較社会文化」 九州大学大学院比較社会文化学府 20 1 - 10 1341-1659 2014/03 [Refereed]
本稿では、ジルコンの迅速分離手法とLA-ICP-MSを用いたU-Pb年代測定の実例を報告する。ジルコンは岩石中には副成分鉱物として産するため、その量的な問題から多くの場合、試料からの分離が必要となる。ジルコンの分離には、現在においても重液を用いた分離法が一般的である。しかしながら、重液の使用に対する非効率性や人体に及ぼす危険性、高コストが指摘されてきた。そこで、小論ではこれらの問題を解決するために、重液を用いないジルコンの迅速分離手法を考案した。本手法では、粉末試料をビーカーや時計皿による水簸および椀掛けをすることでジルコンを30分以内に抽出することが可能であり、重液分離と比べると極めて迅速で効率よく、低コストで安全な手法といえる。ジルコンはU-Pb年代測定のほかに、包有物解析や化学組成から様々な地質事変を制約できる鉱物である。本手法は膨大なジルコン分析に対応した地質学的研究に非常に有用な手法であるとともに考古学などの他分野への応用も期待される。This report provides the rapid separation techniques of zircons and an example of U-Pb dating of the zircons using LA-ICP-MS. Zircons have been commonly separated from a sample using heavy liquid. However, previous reports have pointed out the inefficiency, harmful effect and high cost of the heavy liquid method. In this report, we provide the rapid techniques for zircon separation without using heavy liquid, and procedures just before zircon analysis, including separation, hand picking, mounting, and observation under cathodoluminescence image. In the method introduced here, the zircons can be separated only for 30 minutes per one sample just by panning with a beaker and watch glass. Therefore, this method is more efficient, quicker, lower cost and safer compared with heavy liquid separation. - Yasuhito OSANAI, Aya YOSHIMOTO, Nobuhiko NAKANO, Tatsuro ADACHI, Ippei KITANO, Kazuhiro YONEMURA, Jun SASAKI, Nobutaka TSUCHIYA, Hideo ISHIZUKAJapanese Magazine of Mineralogical and Petrological Sciences 43 (3) 71 - 99 1345-630X 2014 [Refereed]
- Yasuhito Osanai, Yoshifumi Nogi, Sotaro Baba, Nobuhiko Nakano, Tatsuro Adachi, Tomokazu Hokada, Tsuyoshi Toyoshima, Masaaki Owada, Madhusoodhan Satish-Kumar, Atsushi Kamei, Ippei KitanoPrecambrian Research 234 8 - 29 0301-9268 2013/09 [Refereed]
The Sor Rondane Mountains of eastern Dronning Maud Land, East Antarctica can be subdivided into two different crustal terranes: the NE-terrane and the SW-terrane. The former is underlain by basement rocks of amphibolite-facies (unit A) and granulite-facies (unit B), and the latter by granulite-facies (unit C) to greenschist-facies (units D and D') rocks. The metamorphic evolution of the NE-terrane exhibits a clockwise pressure-temperature-time (P-T-t) path and the SW-terrane exhibits a counter-clockwise P-T-t path, and detrital zircon U-Pb ages are also different between the two terranes. The differences in the metamorphic evolution processes and detrital zircon provenance in these two regions can be explained by the collision of the NE-terrane and the SW-terrane which is constrained to have occurred at 600-650 Ma. The collision is interpreted to reflect convergence between the East Maud-East African orogen terrane and the Maud-Nampula terrane of the Kalahari Craton, which are bounded by the Main Tectonic Boundary and passes through the Sor Rondane Mountains. The RTP magnetic anomalies suggest this suture is cut by the subsequent collision boundary between the Kalahari Craton and the Rayner Belt, which is exposed in the Lutzow-Holm region. This collisional belt is considered to have formed at approximately 520-580 Ma. (C) 2013 Elsevier B.V. All rights reserved. - Ippei Kitano, Takeshi IkedaThe Journal of the Geological Society of Japan The Geological Society of Japan 118 (12) 801 - 809 0016-7630 2012 [Refereed]
The Suo metamorphic rocks of the Asakura area of Fukuoka Prefecture underwent contact metamorphism during the intrusion of granitic magmas in the Cretaceous, forming a contact aureole. This aureole is divided from south to north with ascending metamorphic grade into chlorite, chlorite–biotite, biotite, and andalusite zones, based on pelitic mineral assemblages. The andalusite isograd is defined by a muscovite + quartz = andalusite + K-feldspar + water reaction, based on the coexistence of andalusite and K-feldspar. Garnet–biotite thermometry and garnet–biotite–plagioclase–quartz barometry indicate that the andalusite zone formed at temperatures of 560 ± 50°C and at pressures of 2.3 ± 0.90 kbar. The Suo metamorphic rocks were exhumed to ca. 9 km depth by around 95 Ma, assuming that heat was supplied from the Asakura granodiorite to the north, and reached the surface and were overlain by sediments of the Nogata Group sometime before 44 Ma.
MISC
- 北海道大学総合博物館と極地・北方域研究北野一平 極地 59- (2) 69 -72 2023/09
- 神居古潭巡検参加報告北野一平 日本地質学会News 26- (9) 24 -25 2023/09
- The report of gneisses discovered from the Kanuma city and Nakagawa town in the Tochigi PrefectureIppei Kitano Bulletin of the Tochigi Prefectural Museum. Natural history 39- 7 -14 2022/03 [Not refereed]
- 栃木県立博物館で学ぶ地学北野一平 日本地質学会News 25- (2) 7 -7 2022/02 [Not refereed]
- 第60 次日本南極地域観測の地質調査報告香取拓馬, 豊島剛志, 石川正弘, 北野一平 GSJ 地質ニュース 9- (10) 267 -272 2020/10 [Not refereed]
- Report on the 20162017 (JARE-58) geological field survey of Lützow-Holm Bay, Prince Olav Coast and Enderby LandTomokazu Hokada, Sotaro Baba, Atsushi Kamei, Ippei Kitano, Yoichi Motoyoshi, Prayath Nantasin, Nugroho Imam Setiawan, Davaa-Ochir Dashbaatar Antarctic Record 61- (1) 11 -56 2017The 58th Japanese Antarctic Research Expedition (JARE-58) conducted geological field surveys in the regions of Lützow-Holm Bay, Prince Olav Coast, and Enderby Land during the 20162017 austral summer season. The field party consisted of four Japanese geologists and three Asian geologists (Thai, Indonesian, Mongolian), and was joined periodically by JARE-58 expedition leader, Prof. Motoyoshi. Field parties were supported throughout the summer season by a smaller secondary helicopter (AS350) in addition to two main helicopters (CH101) stationed on the icebreaker Shirase. This report summarizes field preparations and the geological work undertaken, and highlights several key points for future planning and research.
Books etc
Presentations
- Monazite dating of pelitic gneisses in the Dai Loc Complex, Truong Son Belt, VietnamBui, T.S.V, Kitano, I, Osanai, Y, Nakano, NInternational Association for Gondwana Research 2023 Convention and 20th International Conference on Gondwana to Asia 2023/10
- New zircon U–Pb geochronology of high-pressure schists from the Itoigawa-Omi area in the Hida Gaien Belt, JapanKitano, I, Osanai, Y, Tsujimori, T, Takenouchi, K, Nakano, NInternational Association for Gondwana Research 2023 Convention and 20th International Conference on Gondwana to Asia 2023/10
- 山口県東部屋代島の深成岩類の火成活動史：九州地域との比較大和田正明, 宮下由香里, 佐藤大介, 小山内康人, 北野一平日本地質学会第130年学術大会 2023/09
- 東南極リュツォ・ホルム複合岩体のあけぼの岩に産する変花崗岩類をもたらした火成活亀井淳志, 市田花歩, 粟田 晶, 外田智千, 堀江憲路, 竹原真美, 馬場壮太郎, 北野一平, Nugroho I.SETIAWAN, Prayath NANTASIN, Davaa–ochir, DASHBAATAR, 本吉洋一日本地質学会第130年学術大会 2023/09
- 栃木県西部足尾山地に産する片麻岩に含有されるクリソベリルの産状報告と意義北野一平日本地質学会第130年学術大会 2023/09
- 栃木県西部足尾山地から見出された片麻岩の温度圧力条件北野一平日本地質学会第130年学術大会 2023/09
- 東南極リュツォ・ホルム岩体の天文台岩に産する変花崗岩類をもたらした火成活動亀井淳志, 市川もも, 外田智千, 谷健一郎, 北野一平, 馬場壮太郎, Nugroho I.SETIAWAN, Prayath NANTASIN, Davaa–ochir, DASHBAATAR, 本吉洋一日本鉱物科学会2023年年会 2023/09
- 日高山脈ソガベツ沢のマイロナイト化した泥質グラニュライトの温度圧力経路北野一平日本地質学会北海道支部2023年度例会 2023/06
- Hf-isotope of UHT metamorphic rocks from the Napier Complex, East Antarctica: How to relate with Sri Lankan Highland Complex? [Invited]Osanai, Y, Kitano, I39th Annual Technical Sessions and Annual General Meeting of Geological Society of Sri Lanka (GSSL) 2023/02
- The Western Rayner Complex – connection between Dronning Maud Land and Enderby Land, East AntarcticaHokada, T, Baba, S, Kamei, A, Kitano, I, Horie, K, Takehara, MThe Thirteenth Symposium on Polar Science 2022/11
- The pressure-temperature conditions of high-grade pelitic gneisses in the Dai Loc Complex, Truong Son Belt, central VietnamKitano, I, Bui, T.S.V, Osanai, Y, Nakano, N, Pham, B, Hokada, TThe Thirteenth Symposium on Polar Science 2022/11
- 九州黒瀬川構造帯・超高温変ハンレイ岩類の変成作用と変成年代小山内康人, 中野伸彦, 北野一平, 大和田正明, Bui Thi Sinh Vuong, Boldbaatar Dolzodmaa日本鉱物科学会2022年年会 2022/09
- 北関東栃木県西部の足尾帯から見出された片麻岩の記載岩石学的特徴と地質学的意義北野一平日本地質学会第129年学術大会 2022/09
- Petrology and zircon U–Pb geochronology of pelitic gneisses and granitoids from the Dai Loc Complex in the Truong Son Belt, VietnamBui, T.S.V, Osanai, Y, Nakano, N, Kitano, I, Adachi, T, Tran, T.A, Binh, P, Ngoc, C.PVirtual Regional Geoscience Congress of Southeast Asia (GEOSEA) XVI and GeoCon 2021 2021/12
- Ancient earthquakes and E-W compressional stress field recorded by brittle faults and pseudotachylytes from southwestern Skarvsnes in the Lützow-Holm Complex, East AntarcticaToyoshima, T, Kitano, I, Ishikawa, M, Katori, T, Hokada, TThe Twelfth Symposium on Polar Science 2021/11
- Monazite U-Th-Pb ages of the “unnamed nunatak (Nunatak 170224-3)” east of Forfinger Point, Western Rayner Complex, Enderby Land, East AntarcticaHokada, T, Baba, S, Kamei, A, Kitano, IThe Twelfth Symposium on Polar Science 2021/11
- Kitano, I, Hokada, T, Baba, S, Kamei, A, Motoyoshi, Y, Toyoshima, T, Ishikawa, M, Katori, T, Nakano, N, Osanai, YThe Twelfth Symposium on Polar Science 2021/11
- 中部九州阿蘇カルデラ北部合戦群地域に露出する泥質片麻岩および花崗岩のジルコンU–Pb年代北野一平, 小山内康人, 北村圭吾, 中野伸彦日本地質学会第128年学術大会 2021/09
- 東南極プリンス・オラフ海岸，あけぼの岩に分布するザクロ石黒雲母片麻岩のジルコンU–Pb年代馬場壮太郎, 堀江憲路, 外田智千, 竹原真美, 亀井淳志, 北野一平, 本吉洋一日本地質学会第128年学術大会 2021/09
- ミャンマー・モゴック北方に見出されるUHT変成岩Khaing, H, 小山内康人, 中野伸彦, Dolzodomaa, B, 北野一平, Zaw, H, 足立達朗, 大和田正明日本鉱物科学会2021年年会 2021/09
- Fossil earthquake recorded by pseudotachylytes and two textural types of cataclasites from northern Langhovde in the Lützow-Holm Complex, East AntarcticaToyoshima, T, Kitano, I, Ishikawa, M, Katori, T, Hokada, TThe Eleventh Symposium on Polar Science 2020/12
- Geochemical study on charnockites in Rundvågshetta, Lützow-Holm ComplexKamei, A, Awata, H, Hokada, T, Baba, S, Kitano, I, Motoyoshi, YThe Eleventh Symposium on Polar Science 2020/12
- Geologic nature and evolution of Western Rayner Complex, with reference to Point Widdows charnockite and its localized hydration processHokada, T, Baba, S, Kamei, A, Kitano, I, Motoyoshi, YThe Eleventh Symposium on Polar Science 2020/12
- Cordierite megacrysts in felsic gneiss from Botunnuten in southern Lützow-Holm Complex, East AntarcticaBaba, S, Ohshiro, S, Hokada, T, Kamei, A, Kitano, I, Motoyoshi, YThe Eleventh Symposium on Polar Science 2020/12
- Kitano, I, Toyoshima, T, Ishikawa, M, Katori, T, Hokada, TThe Eleventh Symposium on Polar Science 2020/12
- Kitano, I, Hokada, T, Baba, S, Kamei, A, Motoyoshi, YThe Eleventh Symposium on Polar Science 2020/12
- Ultrahigh-temperature metamorphic rocks from Highland Complex, Sri LankaOsanai, Y, Nakano, N, Kitano, I, Adachi, T, Owada, M, Sajeev, K, Kehelpannala, W, Malaviachchi, SMAESA Second International Conference on Applied Earth Sciences in Myanmar and Neighboring Regions 2019/12
- Permo–Triassic tectonic processes in Kannak Complex, Kon Tum Massif, VietnamOwada, M, Osanai, Y, Nakano, N, Kitano, I, Adachi, TMAESA Second International Conference on Applied Earth Sciences in Myanmar and Neighboring Regions 2019/12
- Geological field survey in the regions of the Lützow-Holm Bay, Prince Olav Coast and Enderby Land, 2018-2019 (JARE-60)Toyoshima, T, Ishikawa, M, Kitano, I, Katori, T, Hokada, TThe Tenth Symposium on Polar Science 2019/12
- Pseudotachylytes from Langhovde and Skarvsnes in the Lützow-Holm Complex, East Antarctica, and their conditions of formationToyoshima, T, Ishikawa, M, Kitano, I, Katori, T, Hokada, TThe Tenth Symposium on Polar Science 2019/12
- Geological connection between Dronning Maud Land and Enderby LandHokada, T, Horie, K, Baba, S, Kamei, A, Kitano, I, Motoyoshi, Y, Hiroi, Y, Takehara, M, Shiraishi, KThe Tenth Symposium on Polar Science 2019/12
- Zircon chronology for high temperature metamorphic rocks in the Wanni and Highland Complexes, Sri LankaKitano, I, Osanai, Y, Nakano, N, Adachi, T2019 Internal Association for Gondwana Research Annual Convention & 16th International Symposium on Gondwana to Asia 2019/11
- Newly determined U¬-Pb zircon ages from the Napier Complex, East AntarcticaOsanai, Y, Kitano, I, Nakano, N, Adachi, T, Toyoshima, T, Hokada, T, Owada, M, Tsunogae, T, Bui, T.S.V2019 Internal Association for Gondwana Research Annual Convention & 16th International Symposium on Gondwana to Asia 2019/11
- Metamorphic and geochronological records in Rayner and Western Rayner Complexes, East Antarctica: Implications for Dronning Maud Land (Maud Province) – Enderby Land (Rayner Province) connectionHokada, T, Horie, K, Baba, S, Kamei, A, Kitano, I, Motoyoshi, Y, Hiroi, Y, Takehara, M, Shiraishi, K2019 Internal Association for Gondwana Research Annual Convention & 16th International Symposium on Gondwana to Asia 2019/11
- New insights into the metamorphic evolution of the Lützow-Holm Complex along the Prince Olav Coast, East AntarcticaBaba, S, Hokada, T, Kamei, A, Kitano, I, Motoyoshi, Y, Nantasin, P, Setiawan, N, Dashbaatar, D2019 Internal Association for Gondwana Research Annual Convention & 16th International Symposium on Gondwana to Asia 2019/11
- Metamorphic history of the high-grade metamorphic rocks in the Ngoc Linh Complex, Kontum Massif, VietnamBui, T.S.V, Osanai, Y, Nakano, N, Adachi, T, Kitano, I, Owada, M2019 Internal Association for Gondwana Research Annual Convention & 16th International Symposium on Gondwana to Asia 2019/11
- 山口県長門構造帯に産する変成岩・深成岩類のジルコンU–Pb年代の特徴北野一平, 小山内康人, 中野伸彦, 足立達朗, 加藤涼介, Bui Thi Sinh Vuong日本鉱物科学会2019年年会 2019/09
- 北野一平, 小山内康人, 中野伸彦, 足立達朗日本鉱物科学会2019年年会 2019/09
- 西南日本九州北部に分布する三郡変成帯結晶片岩の砕屑性ジルコン後背地の多様性北野一平, 小山内康人, 中野伸彦, 足立達朗日本鉱物科学会2019年年会 2019/09
- 八幡浜大島に分布する大島変成岩体のLA-ICP-MSジルコンU–Pb年代と地体構造上の意義小山内康人, 北野一平, 中野伸彦, 足立達朗, Bui Thi Sinh Vuong, 小松正幸日本鉱物科学会2019年年会 2019/09
- ベトナム・コンツム地塊，カンナック岩体，ペルム紀－三畳紀，火成作用と変成作用の関係大和田正明, 小山内康人, 中野伸彦, 北野一平, 足立達朗日本鉱物科学会2019年年会 2019/09
- Zircon-monazite-garnet behaviours during high-grade metamorphism in the Kontum Massif, VietnamBui Thi Sinh Vuong, 小山内康人, 中野伸彦, 足立達朗, 北野一平, 大和田正明日本鉱物科学会2019年年会 2019/09
- 東南極プリンス・オラフ海岸に分布する泥質片麻岩の変成条件馬場壮太郎, 外田智千, 亀井淳志, 北野一平, 本吉洋一日本地質学会第126年学術大会 2019/09
- Re-examination of metamorphic and geochronologic events in Rayner Complex and Western Rayner Complex in AntarcticaHokada, T, Baba, S, Kamei, A, Kitano, I, Horie, K, Hiroi, Y, Motoyoshi, Y, Takehara, M, Shiraishi, KJapan Geoscience Union Meeting 2019 2019/05
- Rayner Complex and Western Rayner Complex in Enderby LandHokada, T, Baba, S, Kamei, A, Kitano, I, Horie, K, Motoyoshi, Y, Hiroi, Y, Shiraishi, K, Takehara, MThe Ninth Symposium on Polar Science 2018/12
- Formation of shear zone in Akebono Rock, Prince Olav Coast, East AntarcticaBaba, S, Hokada, T, Kamei, A, Kitano, I, Motoyoshi, Y, Nantasin, P, Setiawan, N, Dashbaatar, DThe Ninth Symposium on Polar Science 2018/12
- Igneous activity of Middle Proterozoic meta-tonalite in Cape Hinode, Prince Olav Coast, East AntarcticaKamei, A, Tashima, H, Hokada, T, Baba, S, Kitano, I, Hiroi, Y, Motoyoshi, YThe Ninth Symposium on Polar Science 2018/12
- Geochemical comparison of eastern and western meta-igneous rocks from Lützow-Holm Complex, East AntarcticaAwata, H, Kamei, A, Hokada, T, Baba, S, Kitano, I, Dashbaatar, D, Setiawan, N, Nantasin, P, Motoyoshi, YThe Ninth Symposium on Polar Science 2018/12
- Preliminary report for zircon geochronology of tonalitic gneiss at an unnamed nunatak in western part of the Napier Complex, East AntarcticaHorie, K, Takehara, M, Hokada, T, Baba, S, Kamei, A, Kitano, I, Nantasin, P, Setiawan, N, Dashbaatar, D, Motoyoshi, YThe Ninth Symposium on Polar Science 2018/12
- Elemental redistribution in zircons of felsic gneiss from the Harvey Nunatak in the Napier Complex, East AntarcticaTakehara, M, Horie, K, Hokada, T, Baba, S, Kamei, A, Kitano, I, Nantasin, P, Setiawan, N, Dashbaatar, D, Motoyoshi, YThe Ninth Symposium on Polar Science 2018/12
- 東南極ナピア岩体ハーベイヌナタークに産する珪長質片麻岩中のジルコンの地球化学竹原真美, 堀江憲路, 外田智千, 馬場壮太郎, 亀井淳志, 北野一平, Nantasin Prayath, Setiawan Nugroho, Dashbaatar Davaa-ochir, 本吉洋一日本地球化学会第65回年会 2018/09
- スリランカ・ハイランド岩体およびワンニ岩体に分布する変成火成岩のインヘリテッドジルコンHf同位体組成北野一平, 小山内康人, 中野伸彦, 足立達朗日本鉱物科学会2018年年会 2018/09
- U¬–Pb age and REE chemistry of zircons in pelitic gneisses from the Higo metamorphic Belt, Japan: Implication for timing of high-temperature metamorphismBui Thi Sinh Vuong, 小山内康人, 中野伸彦, 足立達朗, 北野一平日本鉱物科学会2018年年会 2018/09
- 西南日本内帯高圧変成岩類の同位体年代学田淵洸太郎, 石塚英男, 小山内康人, 中野伸彦, 足立達朗, 北野一平日本鉱物科学会2018年年会 2018/09
- Protolith characteristics and tectonic implications for high-grade metamorphic rocks in the Highland and Wanni Complexes, Sri LankaKitano, I, Osanai, Y, Nakano, N, Adachi, TJapan Geoscience Union Meeting 2018 2018/05
- New geochronological report of tonalitic gneisses at Harvey Nunatak and Mt. Reed in western part of Napier Complex, East AntarcticaTakehara, M, Horie, K, Hokada, T, Baba, S, Kamei, A, Kitano, I, Nantasin, P, Setiawan, N, Dashbaatar, D, Motoyoshi, YJapan Geoscience Union Meeting 2018 2018/05
- Re-examination of metamorphic and geochronologic events in eastern Dronning Maud Land and Enderby Land, East Antarctica: current status and future perspectivesHokada, T, Baba, S, Kamei, A, Kitano, I, Nantasin, P, Setiawan, N, Dashbaatar, D, Motoyoshi, Y, Hiroi, Y, Osanai, Y, Horie, K, Takehara, M, Shiraishi, KJapan Geoscience Union Meeting 2018 2018/05
- Petrology and geochemistry of Middle Proterozoic meta-tonalite in Cape Hinode, Prince Olav Coast, East AntarcticaKamei, A, Tashima, H, Hokada, T, Baba, S, Kitano, I, Hiroi, YJapan Geoscience Union Meeting 2018 2018/05
- Protolith of orthogneiss and amphibolite in Akebono Rock, Prince Olav Coast, East AntarcticaKurita, A, Kamei, A, Hokada, T, Baba, S, Kitano, I, Dashbaatar, D, Setiawan, N, Nantasin, PJapan Geoscience Union Meeting 2018 2018/05
- Timing of metamorphic events in the Wanni and Highland Complexes, Sri LankaKitano, I, Osanai, Y, Nakano, N, Adachi, TThe Eighth Symposium on Polar Science 2017/12
- Metamorphism in Akebono Rock, Prince Olav Coast, East AntarcticaBaba, S, Hokada, T, Kamei, A, Kitano, I, Motoyoshi, Y, Nantasin, P, Setiawan, N, Dashbaatar, DThe Eighth Symposium on Polar Science 2017/12
- Preliminary report for zircon geochronology of tonalitic gneiss at Mt. Reed in western part of the Napier Complex, East AntarcticaHorie, K, Takehara, M, Hokada, T, Baba, S, Kamei, A, Kitano, I, Nantasin, P, Setiawan, N, Dashbaatar, D, Motoyoshi, YThe Eighth Symposium on Polar Science 2017/12
- First geochronological report of tonalitic gneiss at Harvey Nunatak in western part of the Napier Complex, East AntarcticaTakehara, M, Horie, K, Hokada, T, Baba, S, Kamei, A, Kitano, I, Nantasin, P, Setiawan, N, Dashbaatar, D, Motoyoshi, YThe Eighth Symposium on Polar Science 2017/12
- Participation of Indonesia in Japanese Antarctic Research Expedition-58 2016-2017, Progress and Current Influences after the ExpeditionSetiawan, N, Hokada, T, Baba, S, Kamei, A, Kitano, I, Motoyoshi, Y, Nantasin, P, Dashbaatar, DThe Eighth Symposium on Polar Science 2017/12
- Chalcopyrite-pyrite mineralization associated with Precambrian trondhjemite-metagabbro intrusions, in the Skallevikhalsen of Lutzow-Holm Bay, Eastern AntarcticaDashbaatar, D, Motoyoshi, Y, Hokada, T, Baba, S, Kamei, A, Kitano, I, Nantasin, P, Setiawan, NThe Eighth Symposium on Polar Science 2017/12
- スリランカ・ハイランド岩体およびワンニ岩体に分布する高温変成岩の地球化学的・年代学的特徴と形成テクトニクス北野一平, 小山内康人, 中野伸彦, 足立達朗日本鉱物科学会2017年年会 2017/09
- 東南極プリンス・オラフ海岸，あけぼの岩の変形変成作用馬場壮太郎, 外田智千, 亀井淳志, 北野一平, 本吉洋一日本地質学会第124年学術大会 2017/09
- 東南極ドロンイングモードランド東部からエンダビーランドに分布する太古代-原生代の高温変成岩類：2016-2017調査報告外田智千, 馬場壮太郎, 亀井淳志, 北野一平, Prayath Nantasin, Nugroho Setiawan, Davaa-ochir Dashbaatar, 本吉洋一日本地質学会第124年学術大会 2017/09
- Trace element partitioning during partial melting in main zone of the Hidaka metamorphic beltKato, R, Osanai, Y, Nakano, N, Adachi, T, Kitano, IJapan Geoscience Union Meeting 2017 2017/05
- Tectono-metamorphic evolution of the Kurosegawa tectonic belt in Southwest JapanOsanai, Y, Nakano, N, Adachi, T, Kitano, I, Yoshimoto, A, Kato, R, Tsuchiya, N, Ishizuka, HJapan Geoscience Union Meeting 2017 2017/05
- スリランカ・ハイランド岩体およびワンニ岩体に分布する高温変成岩の全岩化学組成北野一平, 小山内康人, 中野伸彦, 足立達朗日本鉱物科学会2016年年会 2016/09
- 南部北上山地，氷上花崗岩類の結晶作用と成因佐々木惇, 土谷信高, 足立達朗, 中野伸彦, 北野一平, 小山内康人, 足立佳子日本地球惑星科学連合2016年大会 2016/05
- LA-ICP-MS Zircon U-Pb ages for metamorphic rocks from the Highland and Wanni Complexes, Sri LankaKitano, I, Osanai, Y, Nakano, N, Adachi, TJapan Geoscience Union Meeting 2016 2016/05
- Petrological and chronological constraints of UHT granulites from Highland Complex, Sri Lanka: implications on Gondwana correlationOsanai, Y, Sajeev, K, Nakano, N, Kitano, I, Kehelpannala, W, Kato, R, Adachi, T, Malaviarachchi, S.P.KJapan Geoscience Union Meeting 2016 2016/05
- Late Permian plume-related magmatism and tectonothermal events in the Kontum Massif, central VietnamOwada, M, Osanai, Y, Nakano, N, Adachi, T, Kitano, I, Tran, T, Kigali, HJapan Geoscience Union Meeting 2016 2016/05
- 日高変成帯主帯における苦鉄質変成岩の部分溶融加藤涼介, 小山内康人, 中野伸彦, 足立達朗, 北野一平, 加々島慎一日本地質学会第122年学術大会 2015/09
- 氷上花崗岩類と古生代花崗岩類のSr-Nd同位体比佐々木惇, 土谷信高, 柴田知之, 芳川雅子, 足立達朗, 中野伸彦, 北野一平, 小山内康人日本地質学会第122年学術大会 2015/09
- スリランカ・西および東ハイランド岩体に分布する高温変成岩類のLA-ICP-MSジルコンU-Pb年代北野一平, 小山内康人, 中野伸彦, 足立達朗日本鉱物科学会2015年年会 2015/09
- LA-ICP-MS Zircon U-Pb ages from metamorphic rocks in the southwestern part of Highland Complex, Sri LankaKitano, I, Osanai, Y, Nakano, N, Adachi, TJapan Geoscience Union Meeting 2015 2015/05
- スリランカ・Highland Complex中央部に分布する変成岩のLA-ICP-MSジルコンU-Pb年代北野一平, 小山内康人, 中野伸彦, 足立達朗, Sanjeewa, P, K. Malaviarachchi, P. L. Dharmapriya日本地質学会第121年学術大会 2014/09
- 黒瀬川構造帯に分布する花崗岩類および変ハンレイ岩の年代学的特徴小山内康人, 吉本紋, 中野伸彦, 足立達朗, 北野一平, 米村和紘, 佐々木惇, 土谷信高, 石塚英男日本地質学会第121年学術大会 2014/09
- 東南極セールロンダーネ山地に分布する変成岩類の全岩化学組成とジルコンU-Pb年代北野一平, 小山内康人, 中野伸彦, 足立達朗日本鉱物科学会2014年年会 2014/09
- 黒瀬川構造帯に分布する高圧変成岩，高温変成岩および花崗岩の年代学的特徴と形成テクトニクス吉本紋, 小山内康人, 中野伸彦, 足立達朗, 北野一平, 米村和紘, 石塚英男日本鉱物科学会2014年年会 2014/09
- 黒瀬川帯に分布する蛇紋岩中の変成岩および火成岩ブロックの形成テクトニクス吉本紋, 小山内康人, 中野伸彦, 足立達朗, 北野一平, 米村和紘, 石塚英男日本地球惑星科学連合2014年大会 2014/05
- 東南極セールロンダーネ山地に分布する変成岩類の年代学的特徴および全岩化学組成北野一平, 小山内康人, 足立達朗, 中野伸彦日本地質学会第120年学術大会 2013/09
- 東南極セールロンダーネ山地に分布する変成岩類のジルコンLA-ICP-MS U-Pb年代北野一平, 小山内康人, 足立達朗, 中野伸彦日本地球惑星科学連合2013年大会 2013/05
- 東南極セールロンダーネ山地の南部〜東部におけるジルコンのLA-ICP-MS U-Pb年代北野一平, 小山内康人, 足立達朗, 中野伸彦日本地質学会第119年学術大会 2012/09
- 八幡浜大島に分布する大島変成岩類の年代論小山内康人, 中野伸彦, 足立達朗, 北野一平, 米村和紘, 吉本紋, 小松正幸日本地質学会第119年学術大会 2012/09