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Titlebook: Crust/Mantle Recycling at Convergence Zones; Stanley R. Hart,Levent Gülen Book 1989 Kluwer Academic Publishers 1989 atmosphere.chemistry.g

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發(fā)表于 2025-3-21 18:43:17 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Crust/Mantle Recycling at Convergence Zones
編輯Stanley R. Hart,Levent Gülen
視頻videohttp://file.papertrans.cn/241/240485/240485.mp4
叢書名稱Nato Science Series C:
圖書封面Titlebook: Crust/Mantle Recycling at Convergence Zones;  Stanley R. Hart,Levent Gülen Book 1989 Kluwer Academic Publishers 1989 atmosphere.chemistry.g
描述This book consists of a collection of papers presented at the NATO Advanced Research Workshop (ARW) on "Crust/mantle Recycl ing at Convergence Zones," held in Antalya, Turkey, between May 25 to 29, 1987. The workshop was attended by 36 earth scientists from ten countries and 28 papers were presented. Crust/mantle recycling is one of the most fundamental processes in the Earth. The study and understanding of this process requires the consideration of the Earth as a whole system including the atmosphere, the hydrosphere and the core, as well as the crust and the mantle; effective interdisciplinary collaboration is therefore essential to our progress. The Antalya ARW gave us the opportunity to assemble key specialists from relevant branches of the earth sciences and to address our state of knowledge. This ARW proved to be very useful in attaining an interdisciplinary, mutual understanding among specialists from diverse fields such as isotope and trace element geochemistry, mineral physics, theoretical geophysics, seismology, experimental petrology, and structural geology.
出版日期Book 1989
關(guān)鍵詞atmosphere; chemistry; geochemistry; geology; geophysics; mineral; petrology; plate tectonics; structural ge
版次1
doihttps://doi.org/10.1007/978-94-009-0895-6
isbn_softcover978-94-010-6891-8
isbn_ebook978-94-009-0895-6Series ISSN 1389-2185
issn_series 1389-2185
copyrightKluwer Academic Publishers 1989
The information of publication is updating

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Magma Generation in Subduction Zones,phere wedge overlying the subducted slab. Lack of knowledge of the thermal structure of island arc regions has hindered our understanding. By comparing laboratory results with seismic and heat flow observations in island arc regions we determine that temperatures are generally below the solidus.
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Isotopic and Chemical Signatures of Recycled Oceanic and Continental Crust, evolution. Isotopic and chemical constraints show that elements like Rb, U, Th and Pb will have very short residence times (0.1–1.0 Ga) in the mantle and be close to steady state. In contrast, elements like Sr, Nd, Sm, Hf and Lu will have much longer residence times (5–10 Ga) and be far from steady state.
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phere wedge overlying the subducted slab. Lack of knowledge of the thermal structure of island arc regions has hindered our understanding. By comparing laboratory results with seismic and heat flow observations in island arc regions we determine that temperatures are generally below the solidus.
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evolution. Isotopic and chemical constraints show that elements like Rb, U, Th and Pb will have very short residence times (0.1–1.0 Ga) in the mantle and be close to steady state. In contrast, elements like Sr, Nd, Sm, Hf and Lu will have much longer residence times (5–10 Ga) and be far from steady state.
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