Effect of the chemical composition of the crust on the metamorphic evolution of orogenic wedges
Effect of the chemical composition of the crust on the metamorphic evolution of orogenic wedges
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DOI：
10.1046/j.1525-1314.2003.00422.x
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发表时间：
2003-02
影响因子：
3.4
通讯作者：
B. Goffé;R. Bousquet;P. Henry;X. Le Pichon
中科院分区：
文献类型：
--
作者：
B. Goffé;R. Bousquet;P. Henry;X. Le Pichon
岩石学数据提供了一个很好的记录，深刻的侵蚀造山带的热结构，并在原则上，可以用来联系造山带的变质结构，其变形历史。在本文中，我们提出了各种俯冲模型的二维热模拟，考虑到不同的楔形几何形状以及密度和地形的变化与变质反应。
Petrological data provide a good record of the thermal structure of deeply eroded orogens, and, in principle, might be used to relate the metamorphic structure of an orogen to its deformational history. In this paper, we present two‐dimensional thermal modelling of various subduction models taking into account varying wedge geometry as well as variation of density and topography with metamorphic reactions.