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| セッション概要 |
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| 固体地球科学(S) |
| セッション小記号 |
地球内部科学・地球惑星テクトニクス(IT)
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| セッションID |
S-IT05
|
| タイトル |
和文 |
Cause and evolution of plate tectonics: Advances in understanding oceanic plate-continental systems
|
| 英文 |
Cause and evolution of plate tectonics: Advances in understanding oceanic plate-continental systems
|
| タイトル短縮名 |
和文 |
Cause and evolution of plate tectonics
|
| 英文 |
Cause and evolution of plate tectonics
|
| 代表コンビーナ |
氏名 |
和文 |
Becker Thorsten
|
| 英文 |
Thorsten Becker
|
| 所属 |
和文 |
Department of Earth Sciences,
University of Southern California
|
| 英文 |
Department of Earth Sciences,
University of Southern California
|
| メールアドレス |
twb@usc.edu
|
|
共同コンビーナ 1
|
氏名 |
和文 |
Hernlund John
|
| 英文 |
John Hernlund
|
| 所属 |
和文 |
Earth-Life Science Institute
|
| 英文 |
Earth-Life Science Institute
|
| メールアドレス |
hernlund@gmail.com
|
|
共同コンビーナ 2
|
氏名 |
和文 |
中川 貴司
|
| 英文 |
Takashi Nakagawa
|
| 所属 |
和文 |
海洋研究開発機構地球内部ダイナミクス領域
|
| 英文 |
JAMSTEC/IFREE
|
| メールアドレス |
ntakashi@jamstec.go.jp
|
| 国際セッション開催希望 |
国際セッションとしての開催を希望する
|
| 発表主要言語 |
英語
|
| スコープ |
和文 |
Plate tectonics is moderately well described by the behavior of a cold thermal boundary layer in thermal convection. However, Earth's thermal evolution is co-determined by fractionation and the resulting
complexities of a thermo-chemical system. The recent years have seen dramatic advances in our
ability to quantitatively model the behavior of such a system, and there has also been a resurgence
in the analysis of geological, geophysical, and geochemical constraints on plate tectonics over time.
We invite contributions from across the disciplines that speak to the question on how and why plate
tectonics operates on terrestrial planets, including but not limited to: modeling studies of plate generation;
convection studies including continental cycles; plate tectonic reconstruction analysis; geochemical
reservoir evolution; stochastic and deterministic models of mantle structure; deep mantle phase transition dynamics;basal magma ocean dynamics; thermo-chemical pile dynamics; links between solid Earth and exosphere;continent formation and destruction; and long term volatile cycles.
|
| 英文 |
Plate tectonics is moderately well described by the behavior of a cold thermal boundary layer in thermal convection. However, Earth's thermal evolution is co-determined by fractionation and the resulting
complexities of a thermo-chemical system. The recent years have seen dramatic advances in our
ability to quantitatively model the behavior of such a system, and there has also been a resurgence
in the analysis of geological, geophysical, and geochemical constraints on plate tectonics over time.
We invite contributions from across the disciplines that speak to the question on how and why plate
tectonics operates on terrestrial planets, including but not limited to: modeling studies of plate generation;
convection studies including continental cycles; plate tectonic reconstruction analysis; geochemical
reservoir evolution; stochastic and deterministic models of mantle structure; deep mantle phase transition dynamics;basal magma ocean dynamics; thermo-chemical pile dynamics; links between solid Earth and exosphere;continent formation and destruction; and long term volatile cycles.
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| 発表方法希望 |
口頭および（または）ポスターセッション
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| 招待講演 |
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