中国大地构造

出版时间：2011-5  出版社：高等教育出版社  作者：万天丰  页数：501  
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内容概要

　　本书综合了最近30年来的区域地质、石油地质调查成果，作者自己的构造研究原始资料以及中外学者的研究结果（超过1500篇参考文献），论述了中国大陆整个地质历史的构造演化、一系列的构造事件，编制了各个构造时期的13幅中国大陆构造图，概述了中国大陆板块的主要构造特征。《中国大地构造:数据、地图与演化(英文版)》还特别加强了对于中生代－新生代构造与板内变形的讨论，正是这些构造与变形主要控制了矿床和油气藏的形成，并且对于大陆的环境和自然灾害的形成产生巨大的影响。对于一些重要的大地构造理论问题，《中国大地构造:数据、地图与演化(英文版)》也进行了探讨，例如大范围的板内变形的机制问题、岩石圈的厚度变化、地幔羽的存在问题、全球构造的动力学机制问题等，最后作者提出了自己的地幔羽和陨石撞击的工作假说。《中国大地构造:数据、地图与演化(英文版)》可供研究人员、地质学者在大学教学和地质研究中使用，也适合于矿山、石油公司的地质工作者，以及地质类或矿产资源类研究生使用。作者万天丰是中国地质大学（北京）教授。

书籍目录

Introduction
　1.1 Tectonic Events
　1.2 Universal Tectonic Events？
　1.3 Determination of Tectonic Events in the Chinese
Continent
　1.4 Research Principles and Methods for Interpreting Tectonic
Events
　　1.4.1 The Rock Record
　　1.4.2 The Geometry of Rock Deformation
　　1.4.3 The Kinematics of Blocks
　　1.4.4 The Dynamics of Block Deformation
　　1.4.5 The Chronology of Deformation
　　References
Tectonics of Archean and Paleoproterozoic （Before 1.8 Ga）
　2.1 The Eoarchean （EA, 4.6-3.6 Ga）
　2.2 Tectonics from Paleoarchean to Neoarchean （PA-NA, 3.6-2.5
Ga）
　2.3 Tectonics of the Paleoproterozoic （PP, 2.5-1.8 Ga, Ltfliang
Period）
　2.4 Discussion of the Thickness of Continental Crust in the
Archean and Paleoproterozoic
　References
Tectonics of the Mesoproterozoic, Neoproterozoie and Early Cambrian
（1.8 Ga-513 Ma）
　3.1 Tectonics of the Mesoproterozoic （1,800-1,000 Ma, Changcheng
Period-Jixianian Period）
　3.2 Tectonics of the Qingbaikou Period （1,000-800 Ma）
　3.3 Tectonics of the Nanhua Period （800-680 Ma）
　3.4 Tectonics of the Sinian Period-Early Cambrian Epoch （680-513
Ma）
　3.5 Chinese Continental Blocks in Mesoproterozoic and
Neoproterozoic Global Evolution
　References
Tectonics of Middle Cambrian-Early Devonian（The Qilian Tectonic
Period, 513-397 Ma）
　4.1 Sedimentation, Paleogeography and Paleontology
　4.2 Palaeomagnetism and Palaeotectonic Reconstruction
　4.3 Rock Deformation, Metamorphism and Stress Field
　4.4 Magmatism and Rates of Plate Movement
　4.5 Division of Tectonic Units in Early Paleozoic
　References
Tectonics of Middle Devonian-Middle Permian（The Tianshan Tectonic
Period, 397-260 Ma）
　5.1 Sedimentation, Paleogeography and Paleontology
　5.2 Paleomagnetism and Paleotectonic Reconstruction
　5.3 Rock Deformation, Metamorphism and Stress Field
　5.4 Magmatism and Rates of Plate Movement
　5.5 Tectonics and Plate Movement from the Mesoproterozoic to the
Paleozoic
　References
Tectonics of Late Permian-Triassic（The Indosinian Tectonic Period,
260-200 Ma）
　6.1 Sedimentary Paleogeography
　6.2 Collision Tectonics
　6.3 Intraplate Deformation
　References
7 Tectonics of Jurassic-Early Epoch of Early Cretaceous（The
Yanshanian Tectonic Period, 200-135 Ma）
　7.1 Movement and Rotation of Chinese Continent
　7.2 Intraplate Deformation and the Stress Field
　7.3 Tectono-magmatism in Crust
　References
8 Tectonics of Middle Epoch of Early Cretaceous-Paleocene （The
Sichuanian Tectonic Period, 135-56 Ma）
　8.1 Intraplate Deformation and the Stress Field
　8.2 Tectono-magmatism
　8.3 Formation of the Bangongco-Nujiang Collision Zone and
Northward Movement of the Plates
　References
Tectonics of Eocene-Oligocene （The North Sinian Tectonic Period,
56-23 Ma）
　9.1 Intraplate Deformation, Stress Field and Magmatism
　9.2 Development of the Eastern Basins and Accumulations of Oil and
Gas
　9.3 Formation of the Western Pacific Subduction Zone and Yarlung
Zangbo Collision Zone
　References
10 Tectonics of Miocene-Early Pleistocene （The Himalayan Tectonic
Period, 23-0.78 Ma）
　10.1 Thin-skinned Tectonics, the Formation of the Himalayan Thrust
Zone and the Uplift of the Qinghai-Xizang （Tibet） Plateau
　10.2 Intraplate Deformation, Extension and Dispersion in Eastern
China
　10.3 Formation of Giant Step in Landscape and Extension Basins in
Continental Margin
　References
11 Tectonics of Middle Pleistocene——Holocene （The Neotectonic
Period, since 0.78 Ma）
　11.1 Intraplate Deformation and Recent Tectonic Stress Field
　11.2 The Influence of Recent Tectonic Stress Field on the
Earthquakes, Resources and Environment
　11.3 Dynamic Mechanism of the Recent Tectonic Stress Field
　References
　……

章节摘录

版权页：插图：chondritic meteorites, but icy planetismals may have contributed components of the atmosphere andhydrosphere. By analogy with the evolution of the moon, the growth of the terrestrial mass and volumeresulting from meteorite impact and accretion occurred exponentially over a period of about 50 millionyears （Ouyang ZY et al., 2002）. After 4.0 Ga the number of meteorite impacts decreased very rapidly,and the augmentation of the Earth's mass since that time, caused by the impacts, has been only 1025grams, 1/600 of its total mass. This implies that accretion of the Earth effectively ceased at about 4.0 Ga,and the mass and volume of the Earth has since remained essentially unchanged.

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