《CRUST-MANTLE THERMAL STRUCTURE AND TECTONOTHERMAL EVOLUTION OF THE TIBETAN PLATEAU》是1996年科學出版社出版的圖書，作者是Shen Xianjie。
基本介紹
- 中文名：CRUST-MANTLE THERMAL STRUCTURE AND TECTONOTHERMAL EVOLUTION OF THE TIBETAN PLATEAU
- 作者：Shen Xianjie
- 出版社：科學出版社
- 出版時間：1996年1月
- ISBN：7030052714
內容簡介,圖書目錄,
內容簡介
This monograph specialized in the thermnal therme of the Tibetan mechanics in its geological evolution is dedicated to systematic studies on all relevant thermal aspects including the terrestrial heat flow measurements, the distribution patterm of the observed heat flow along a NS profile, the crust -mantle thermal structure and its North MiddleSouth triple heterogeneity across the whole plateau. The main emphasishas been put on the close correlation between thermal and comprehensive geophysical fields and the intrinsic genetic linkage between tectonic deformation of terranes and thereby induced deep-seated and superficial thermal activities and responses. Such a brand- new approach combined with substantial absorption of available geoscientific achievements in geology, geophysics and geochemistry of Tibetan researches has been utimately developed into a synthetic idea of integrated tectonothermal evolution of the Tibetan Plateau. Fnally, a new prminent feature of coexisting thick and warm crust is identified in addition to the world-famous mysteries of the successive amalgamation of terranes, the extremely thick crust and the rapid and accelerating uplift of the Tibetan Plateau.
圖書目錄
Foreword
Preface
CONTENTS
Chapter Ⅰ A Brief Outline of Previous Studies Relevant to the Tibetan Tectonothermal Evolution
Chapter Ⅱ Results of Heat Flow Measurements on the Tibetan Plateau and Their Quality Evaluation
Chapter Ⅲ Heat Flow Distribution Pattern and the Crust-Mantle Thermal Structure of the Tibetan Plateau
Chapter Ⅳ Methodology of the Study on the Integrated Tectonothermal Evolution of the Tibetan Plateau
Chapter Ⅴ Tectonic Framework of the 3D Terrane Deformations Constrained by the Surface Uplift History
Chapter Ⅵ Simulation of the Integrated Tectonothermal Evolution and the Main Results
Conclusions
References
