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- W2373040912 abstract "In order to assess the conditions of stress leading to post-orogenic extensions, thetemperature and distribution of stress strength after continental collision are calculated. Thecalculations assume that heat is from radiogenic heat, strain-induced and adiabatic heat andtransported by conduction and either that the lithosphere is homogeneously thickened or thatonly the crust is thickened during collision. Distribution of stress strength and its evolutionat the different parts of collision belts are calculated unger different parameters. Because thestress strength of the lithosphere obviously decreases after homogeneous thickening in 40Maat the center of collision belts, Cordilleras- type extension and delamination at the 40-60 kmand 120-150 km depth due to stretch stress, are possiblly induced. Before delamination,strain-soften mantle-root of the lithosphere and the lower crust control the tectonic style ofMoho and the upper crust. The inner part of compressive stress region, breeding partialstretch stress after thickening between 0 to 10 Ma years, appears Himalayas -typeextension. However, when the width of orogenic belts exceeds by 1000 km, the occurrence ofpost-orogenic extension has relevance to other large-scale tectonic activization in collisionbelts." @default.
- W2373040912 created "2016-06-24" @default.
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- W2373040912 date "1997-01-01" @default.
- W2373040912 modified "2023-09-23" @default.
- W2373040912 title "DISTRIBUTION OF STRESS AND POST-OROGENIC EXTENSION IN COLLISION BELTS" @default.
- W2373040912 hasPublicationYear "1997" @default.
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