典型文献
Significance of a highly refractory source during subduction initiation to form the Izu-Bonin-Mariana Arc
文献摘要：
The ascendent theory that unifies the Earth Sciences is Plate Tectonics,a regime which is unique to Earth.Other convectively active,solid silicate bodies of our Solar System (Venus,Mars,and Io) are encased in a single deforming "lid";on these,multiple plates and hence plate motions do not exist [1].As Earth's tectonic plates are driven by the sinking of old and cold oceanic lithosphere at subduction zones,understanding how new subduction zones originate is vital for a complete plate tectonic theory.Proposed mechanisms of subduction initiation (SI) are controversial but can be either spontaneous,i.e.,caused by forces originating at the SI site,or induced by ongoing plate motions [2].
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作者姓名：
Scott A.Whattam;Robert J.Stern
作者机构：
Department of Geosciences,King Fahd University of Petroleum and Minerals,Dhahran 31261,Saudi Arabia;Department of Geosciences,University of Texas at Dallas,Richardson,TX 75083-0688,USA
文献出处：
引用格式：
[1]Scott A.Whattam;Robert J.Stern-.Significance of a highly refractory source during subduction initiation to form the Izu-Bonin-Mariana Arc)[J].科学通报（英文版）,2022(02):119-121
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ascendent
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0.674752
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