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Estimates for Peak Shock Pressure Based on Analyses of Planar Deformation Features (PDFs) of Shocked Quartz Grains Derived from K/Pg Boundary Deposit within the Chicxulub Crater.
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- Chang Yu
- Earth and Planetary Science, University of Tokyo
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- Tajika Eiichi
- Complexity Science and Engineering, University of Tokyo
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- Goto Kazuhisa
- Chiba Institute of Techonology, PERC
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- Sekine Yasuhito
- Complexity Science and Engineering, University of Tokyo
Bibliographic Information
- Other Title
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- 衝撃変成石英の平面変形構造(PDFs)分析によるチクシュルーブ・クレーター近傍のイジェクタ経験圧力推定
Description
The Chicxulub Crater, Yucatan Peninsula in Mexico, is one of the largest impact structures on the Earth. However, The details of impact processes of the Chicxulub crater is largely unknown.<br> In this study, we measured and analyzed planar deformation features (PDFs) on shocked quartz grains derived from asteroid impact at the K-Pg boundary deposits both within the Chicxulub crater (Yaxcopoil-1 site) in order to estimate peak shock pressure of ejecta deposited within the Chicxulub crater. We revealed that within and around the crater, from moderately to highly shocked quatrz grains and have been deposited for several days.
Journal
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- Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences
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Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences 2012 (0), 194-, 2012
Japan Association of Mineralogical Sciences
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Details 詳細情報について
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- CRID
- 1390001205547147520
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- NII Article ID
- 130005468345
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- Text Lang
- ja
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- Data Source
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- JaLC
- CiNii Articles
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- Abstract License Flag
- Disallowed