12 results on '"Kimura, Jun-Ichi"'
Search Results
2. Refining the eruptive history of Ulleungdo and Changbaishan volcanoes (East Asia) over the last 86 kyrs using distal sedimentary records
- Author
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McLean, Danielle, Albert, Paul G., Suzuki, Takehiko, Nakagawa, Takeshi, Kimura, Jun-Ichi, Chang, Qing, Macleod, Alison, Blockley, Simon, Staff, Richard A., Yamada, Keitaro, Kitaba, Ikuko, Haraguchi, Tsuyoshi, Kitagawa, Junko, and Smith, Victoria C.
- Abstract
The eruptive histories of Ulleungdo (South Korea) and Changbaishan (North Korea/China border) volcanoes are not well constrained since their proximal stratigraphies are poorly exposed or largely inaccessible. However, determining the past behaviour of these volcanoes is critical since future eruptions are likely to disperse ash over some of the world’s largest metropolitan regions. Alkaline tephra deposits erupted from both centres are routinely identified in marine cores extracted from the Sea of Japan, as well as high-resolution lacustrine records east of the volcanoes. Here, we review the distal ash occurrences derived from Ulleungdo and Changbaishan and provide new data from the Lake Suigetsu (central Honshu, Japan) sediment core, in order to provide a more complete and constrained eruption framework. The intensely-dated Lake Suigetsu archive provides one of the most comprehensive distal eruption records for both centres, despite being located ca. 500 km E of Ulleungdo and ca. 1000 km SSE of Changbaishan. The Suigetsu record is utilised to precisely date and geochemically fingerprint (using major, minor and trace element glass compositions) ash fall events that reached central Honshu. Here, we identify a new non-visible (cryptotephra) layer in the Suigetsu sediments, which reveals a previously unreported explosive event from Changbaishan at 42,750 – 42,323 IntCal13 yrs BP (95.4 % confidence interval). This event is chronologically and geochemically distinct from the B-J (Baegdusan-Japan Basin) tephra reported in the Sea of Japan (ca. 50 ka). Furthermore, we also confirm that the widespread U-Ym tephra erupted from Ulleungdo reached central Japan, and is herein dated to 40,332 – 39,816 IntCal13 yrs BP (95.4 % confidence interval). This terrestrial 14C-derived age of the U-Ym can be used to constrain the chronology of marine records containing the same marker layer. This reviewed and integrated tephrostratigraphic framework highlights the pivotal role that distal sedimentary records can play in evaluating the eruptive histories and hazard potential of Ulleungdo and Changbaishan.
- Published
- 2020
3. Refining the eruptive history of Ulleungdo and Changbaishan volcanoes (East \ud Asia) over the last 86 kyrs using distal sedimentary records
- Author
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McLean, Daniella, Albert, Paul G., Suzuki, Takeshi, Nakagawa, Takeshi, Kimura, Jun-Ichi, Chang, Qing Chang, MacLeod, Alison, Blockley, Simon, Staff, Richard A., Yamada, Keitaro, Kitaba, Ikuko, Haraguchi, Tsuyoshi, Kitagawa, Junko, SG14 Project Members, and Smith, Victoria C.
- Abstract
The eruptive histories of Ulleungdo (South Korea) and Changbaishan (North Korea/China border) volcanoes are not\ud well constrained since their proximal stratigraphies are poorly exposed or largely inaccessible. However, determining\ud the past behaviour of these volcanoes is critical since future eruptions are likely to disperse ash over some of the\ud world’s largest metropolitan regions. Alkaline tephra deposits erupted from both centres are routinely identified in\ud marine cores extracted from the Sea of Japan, as well as high-resolution lacustrine records east of the volcanoes.\ud Here, we review the distal ash occurrences derived from Ulleungdo and Changbaishan and provide new data from the\ud Lake Suigetsu (central Honshu, Japan) sediment core, in order to provide a more complete and constrained eruption\ud framework. The intensely-dated Lake Suigetsu archive provides one of the most comprehensive distal eruption\ud records for both centres, despite being located ca. 500 km E of Ulleungdo and ca. 1000 km SSE of Changbaishan.\ud The Suigetsu record is utilised to precisely date and geochemically fingerprint (using major, minor and trace element\ud glass compositions) ash fall events that reached central Honshu. Here, we identify a new non-visible (cryptotephra)\ud layer in the Suigetsu sediments, which reveals a previously unreported explosive event from Changbaishan at 42,750\ud – 42,323 IntCal13 yrs BP (95.4 % confidence interval). This event is chronologically and geochemically distinct from\ud the B-J (Baegdusan-Japan Basin) tephra reported in the Sea of Japan (ca. 50 ka). Furthermore, we also confirm that\ud the widespread U-Ym tephra erupted from Ulleungdo reached central Japan, and is herein dated to 40,332 – 39,816\ud IntCal13 yrs BP (95.4 % confidence interval). This terrestrial 14C-derived age of the U-Ym can be used to constrain\ud the chronology of marine records containing the same marker layer. This reviewed and integrated tephrostratigraphic\ud framework highlights the pivotal role that distal sedimentary records can play in evaluating the eruptive histories and\ud hazard potential of Ulleungdo and Changbaishan.
- Published
- 2020
4. (2019) New Olivine (MongOl Sh11-2) Reference Material for in situ Microanalysis
- Author
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Batanova, Valentina, Thompson, Jay, Danyushevsky, Leonid, Portnyagin, Maxim, Garbe-Schönberg, Dieter, Kimura, Jun-Ichi, Chang, Qing, Senda, Ryoko, Goemann, Karsten, Campillo, Sylvain, and Sobolev, Alexander
- Published
- 2019
5. 千葉セクション
- Author
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Haneda, Yuki, Hayashi, Hiroki, Hongo, Misato, Horie, Kenji, Hyodo, Masayuki, Igarashi, Atsuo, Ishizuka, Osamu, Irizuki, Toshiaki, Itaki, Takuya, Izumi, Kentaro, Kameo, Koji, Kawamata, Moto, Kawamura, Kenji, Kimura, Jun-Ichi, Kojima, Takahiro, Kubota, Yoshimi, Nakazato, Hiroomi, Nishida, Naohisa, Ogitsu, Itaru, Okada, Makoto, Okuda, Masaaki, Okuno, Jun’ichi, Satoguchi, Yasufumi, Senda, Ryoko, Simon, Quentin, Sueyoshi, Testuo, Shikoku, Kizuku, Suganuma, Yusuke, Sugaya, Manami, Takeshita, Yoshihiro, Takehara, Mami, Watanabe, Masami, Yabusaki, Hisashi, Yoshida, Takeshi, Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut National de la Recherche Agronomique (INRA), Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Collège de France (CdF)-Institut national des sciences de l'Univers (INSU - CNRS)-Aix Marseille Université (AMU)-Institut National de la Recherche Agronomique (INRA), and Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
- Subjects
Global Boundary Stratotype Section and Point (GSSP) ,[SDU]Sciences of the Universe [physics] ,Lower-Middle Pleistocene boundary ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences ,Marine Isotope Stage (MIS) 19 ,Matuyama-Brunhes boundary ,Chiba composite section - Abstract
International audience; We propose the extensively studied Chiba section of the Chiba composite section (CbCS) as the Global Boundary Stratotype Section and Point (GSSP) to define the base of the Middle Pleistocene Subseries and Chibanian Stage. The CbCS is a continuous and expanded marine sedimentary succession within the middle of the Ko-kumoto Formation, Boso Peninsula, Chiba Prefecture. It contains well-preserved pollen, marine micro-and macrofossils, a tightly-defined Matuyama-Brunhes (M-B) paleomagnetic polarity boundary, and numerous tephra beds, allowing the establishment of a robust and precise chronostratigraphic framework across the Lower-Middle Pleistocene boundary. Its deep-marine, open-ocean continental slope setting, coupled with high sedimentation rates with no evidence of abrupt deposition, has resulted in preserving both terrestrial and marine environmental changes in and around Marine Isotope Stage (MIS). We have performed high-resolution oxygen isotope analysis , as well as detailed sedimentological, geochemical, and biostrati-graphic studies of the CbCS, confirming the completeness of the stratigraphic interval spanning the Lower-Middle Pleistocene boundary. The M-B polarity boundary serves as the agreed primary guide for the Lower-Middle Pleistocene boundary, and the CbCS represents one of the most detailed marine sedimentary records yet obtained for this reversal, yielding an astronomical age of. ka with a duration of ca.. kyr. This section therefore offers an exceptional opportunity to calibrate the geological time scale as well as understand the dynamics of the geodynamo. The widespread Byk-E tephra lies close to the reversal, allowing precise regional lithostrati-graphic correlation. The CbCS is easy to access from international airports. The section will be permanently preserved and maintained by the local government as a natural monument. Based on these attributes , the base of the Byk-E tephra bed in the Chiba section is the best horizon for establishing the GSSP that will define the Lower-Middle Pleistocene boundary.
- Published
- 2019
6. Author Correction: Fish proliferation and rare-earth deposition by topographically induced upwelling at the late Eocene cooling event (Scientific Reports, (2020), 10, 1, (9896), 10.1038/s41598-020-66835-8)
- Author
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Ohta, Junichiro, Yasukawa, Kazutaka, Nozaki, Tatsuo, Takaya, Yutaro, Mimura, Kazuhide, Fujinaga, Koichiro, Nakamura, Kentaro, Usui, Yoichi, Kimura, Jun-ichi, Chang, Qing, and Kato, Yasuhiro
- Abstract
金沢大学理工研究域地球社会基盤学系, An amendment to this paper has been published and can be accessed via a link at the top of the paper. © 2020, The Author(s).
- Published
- 2020
7. MongOL Sh11-2: Olivine Refer ence Material for In-situ Microanalysis
- Author
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Batanova, Valentina G., Thompson, Jay Michael, Danyushevsky, Leonid V., Portnyagin, Maxim, Garbe-Schönberg, Dieter, Hauri, Erik, Kimura, Jun-Ichi, Chang, Qing, Senda, Ryoko, Goemann, Karsten, Chauvel, Catherine, Campillo, Sylvain, Ionov, Dmitri A., and Sobolev, Alexander V.
- Published
- 2018
8. Missing western half of the Pacific Plate: Geochemical nature of the Izanagi-Pacific Ridge interaction with a stationary boundary between the Indian and Pacific mantles
- Author
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Miyazaki, Takashi, Kimura, Jun-Ichi, Senda, Ryoko, Vaglarov, Bogdan S., Chang, Qing, Takahashi, Toshiro, Hirahara, Yuka, Hauff, Folkmar, Hayasaka, Yasutaka, Sano, Sakae, Shimoda, Gen, Ishizuka, Osamu, Kawabata, Hiroshi, Hirano, Naoto, Machida, Shiki, Ishii, Teruaki, Tani, Kenichiro, and Yoshida, Takeyoshi
- Abstract
The source mantle of the basaltic ocean crust on the western half of the Pacific Plate was examined using Pb–Nd–Hf isotopes. The results showed that the subducted Izanagi–Pacific Ridge (IPR) formed from both Pacific (180–∼80 Ma) and Indian (∼80–70 Ma) mantles. The western Pacific Plate becomes younger westward and is thought to have formed from the IPR. The ridge was subducted along the Kurile–Japan–Nankai–Ryukyu (KJNR) Trench at 60–55 Ma and leading edge of the Pacific Plate is currently stagnated in the mantle transition zone. Conversely, the entire eastern half of the Pacific Plate, formed from isotopically distinct Pacific mantle along the East Pacific Rise and the Juan de Fuca Ridge, largely remains on the seafloor. The subducted IPR is inaccessible; therefore, questions regarding which mantle might be responsible for the formation of the western half of the Pacific Plate remain controversial. Knowing the source of the IPR basalts provides insight into the Indian–Pacific mantle boundary before the Cenozoic. Isotopic compositions of the basalts from borehole cores (165–130 Ma) in the western Pacific show that the surface oceanic crust is of Pacific mantle origin. However, the accreted ocean floor basalts (∼80–70 Ma) in the accretionary prism along the KJNR Trench have Indian mantle signatures. This indicates the younger western Pacific Plate of IPR origin formed partly from Indian mantle and that the Indian–Pacific mantle boundary has been stationary in the western Pacific at least since the Cretaceous.
- Published
- 2015
9. Matuyama-Brunhes boundary age constrained by SHRIMP U-Pb zircon dating of a widespread tephra
- Author
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Suganuma, Yusuke, Okada, Makoto, Horie, Kenji, Kaiden, Hiroshi, Takehara, Mami, Senda, Ryoko, Kimura, Jun-Ichi, Kawamura, Kenji, Kazaoka, Osamu, and Martin J. Head
- Published
- 2014
10. マダガスカル東部地域における太古代クラトンの再変動
- Author
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ICHIKI, Takashi, ISHIKAWA, Masahiro, OSANAI, Yasuhito, NAKANO, Nobuhiko, ADACHI, Tatsuro, KIMURA, Jun-Ichi, and SENDA, Ryoko
- Abstract
第3回極域科学シンポジウム/第32回極域地学シンポジウム 11月30日(金) 統計数理研究所 3階セミナー室
- Published
- 2012
11. Origin of cross-chain geochemical variation in Quaternary lavas from the northern Izu arc: Using a quantitative mass balance approach to identify mantle sources and mantle wedge processes
- Author
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Kimura Jun-Ichi, Kent Adam J. R., Rowe Michael C., Katakuse Maiko, Nakano Fumi, Hacker Bradley R., van Keken Peter E., Kawabata Hiroshi, and Stern Robert J.
- Subjects
arc basalt ,altered oceanic crust ,mantle ,partial melting ,peridotite ,slab - Published
- 2010
12. Fore-arc basalts and subduction initiation in the Izu-Bonin-Mariana system
- Author
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Regan, Mark K., Ishizuka, Osamu, Stern, Robert J., Kelley, Katherine A., Ohara, Yasuhiko, Blichert-Toft, Janne, Bloomer, Sherman H., Cash, Jennifer, Fryer, Patricia, Hanan, Barry, Hickey-Vargas, Rosemary, Ishii, Teruaki, Kimura, Jun-Ichi, Peate, David W., Rowe, Michael C., Woods, Melinda, Department of Geoscience, University of Iowa [Iowa City], Institute of Geoscience and Geoinformation, Geological Survey of Japan, Geoscience Department, University of Texas at Dallas [Richardson] (UT Dallas), Graduate School of Oceanography [Narragansett], University of Rhode Island (URI), Hydrographic and Ocean Department of Japan, Japan Coast Guard Academy, Laboratoire de Sciences de la Terre (LST), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École normale supérieure - Lyon (ENS Lyon), Oregon State University (OSU), Hawaii Institute of Geophysics and Planetology (HIGP), University of Hawai‘i [Mānoa] (UHM), Department of Geological Sciences [San Diego], San Diego State University (SDSU), Department of Earth Sciences [Miami], Florida International University [Miami] (FIU), Institute for Research on Earth Evolution [Yokosuka] (IFREE), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), NSF : 0827817, 0405651, OCE0001824, NSF MARGINS : OCE0001902, EAR0840862, French Institut National des Sciences de l'Univers : INSU, École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), and Department of Geological Sciences [San Diego State Univ] (Geology SDSU)
- Subjects
fore arc ,ophiolite ,basal t ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences ,Mariana ,geochemistry - Abstract
International audience; Recent diving with the JAMSTEC Shinkai 6500 manned submersible in the Mariana fore arc southeast of Guam has discovered that MORB-like tholeiitic basalts crop out over large areas. These ''fore-arc basalts'' (FAB) underlie boninites and overlie diabasic and gabbroic rocks. Potential origins include eruption at a spreading center before subduction began or eruption during near-trench spreading after subduction began. FAB trace element patterns are similar to those of MORB and most Izu-Bonin-Mariana (IBM) back-arc lavas. However, Ti/V and Yb/V ratios are lower in FAB reflecting a stronger prior depletion of their mantle source compared to the source of basalts from mid-ocean ridges and back-arc basins. Some FAB also have higher concentrations of fluid-soluble elements than do spreading center lavas. Thus, the most likely origin of FAB is that they were the first lavas to erupt when the Pacific Plate began sinking beneath the Philippine Plate at about 51 Ma. The magmas were generated by mantle decompression during near-trench spreading with little or no mass transfer from the subducting plate. Boninites were generated later when the residual, highly depleted mantle melted at shallow levels after fluxing by a water-rich fluid derived from the sinking Pacific Plate. This magmatic stratigraphy of FAB overlain by transitional lavas and boninites is similar to that found in many ophiolites, suggesting that ophiolitic assemblages might commonly originate from near-trench volcanism caused by subduction initiation. Indeed, the widely dispersed Jurassic and Cretaceous Tethyan ophiolites could represent two such significant subduction initiation events.
- Published
- 2010
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