中国大地构造——数据、地图与演化

Introduction　1.1 Tectonic Events　1.2 Universal Tectonic Events？　1.3 Determination of Tectonic Events in the ChineseContinent　1.4 Research Principles and Methods for Interpreting TectonicEvents　　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　　ReferencesTectonics 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, 3.6-2.5Ga）　2.3 Tectonics of the Paleoproterozoic （PP, 2.5-1.8 Ga, LtfliangPeriod）　2.4 Discussion of the Thickness of Continental Crust in theArchean and Paleoproterozoic　ReferencesTectonics of the Mesoproterozoic, Neoproterozoie and Early Cambrian（1.8 Ga-513 Ma）　3.1 Tectonics of the Mesoproterozoic （1,800-1,000 Ma, ChangchengPeriod-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 （680-513Ma）　3.5 Chinese Continental Blocks in Mesoproterozoic andNeoproterozoic Global Evolution　ReferencesTectonics of Middle Cambrian-Early Devonian（The Qilian TectonicPeriod, 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　ReferencesTectonics of Middle Devonian-Middle Permian（The Tianshan TectonicPeriod, 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 thePaleozoic　ReferencesTectonics of Late Permian-Triassic（The Indosinian Tectonic Period,260-200 Ma）　6.1 Sedimentary Paleogeography　6.2 Collision Tectonics　6.3 Intraplate Deformation　References7 Tectonics of Jurassic-Early Epoch of Early Cretaceous（TheYanshanian 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　References8 Tectonics of Middle Epoch of Early Cretaceous-Paleocene （TheSichuanian 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 andNorthward Movement of the Plates　ReferencesTectonics 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 andGas　9.3 Formation of the Western Pacific Subduction Zone and YarlungZangbo Collision Zone　References10 Tectonics of Miocene-Early Pleistocene （The Himalayan TectonicPeriod, 23-0.78 Ma）　10.1 Thin-skinned Tectonics, the Formation of the Himalayan ThrustZone and the Uplift of the Qinghai-Xizang （Tibet） Plateau　10.2 Intraplate Deformation, Extension and Dispersion in EasternChina　10.3 Formation of Giant Step in Landscape and Extension Basins inContinental Margin　References11 Tectonics of Middle Pleistocene——Holocene （The NeotectonicPeriod, since 0.78 Ma）　11.1 Intraplate Deformation and Recent Tectonic Stress Field　11.2 The Influence of Recent Tectonic Stress Field on theEarthquakes, Resources and Environment　11.3 Dynamic Mechanism of the Recent Tectonic Stress Field　References　……

　　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。