中國大地構(gòu)造

內(nèi)容概要

　　本書綜合了最近30年來的區(qū)域地質(zhì)、石油地質(zhì)調(diào)查成果，作者自己的構(gòu)造研究原始資料以及中外學(xué)者的研究結(jié)果（超過1500篇參考文獻(xiàn)），論述了中國大陸整個(gè)地質(zhì)歷史的構(gòu)造演化、一系列的構(gòu)造事件，編制了各個(gè)構(gòu)造時(shí)期的13幅中國大陸構(gòu)造圖，概述了中國大陸板塊的主要構(gòu)造特征?！吨袊蟮貥?gòu)造:數(shù)據(jù)、地圖與演化(英文版)》還特別加強(qiáng)了對(duì)于中生代－新生代構(gòu)造與板內(nèi)變形的討論，正是這些構(gòu)造與變形主要控制了礦床和油氣藏的形成，并且對(duì)于大陸的環(huán)境和自然災(zāi)害的形成產(chǎn)生巨大的影響。對(duì)于一些重要的大地構(gòu)造理論問題，《中國大地構(gòu)造:數(shù)據(jù)、地圖與演化(英文版)》也進(jìn)行了探討，例如大范圍的板內(nèi)變形的機(jī)制問題、巖石圈的厚度變化、地幔羽的存在問題、全球構(gòu)造的動(dòng)力學(xué)機(jī)制問題等，最后作者提出了自己的地幔羽和隕石撞擊的工作假說?！吨袊蟮貥?gòu)造:數(shù)據(jù)、地圖與演化(英文版)》可供研究人員、地質(zhì)學(xué)者在大學(xué)教學(xué)和地質(zhì)研究中使用，也適合于礦山、石油公司的地質(zhì)工作者，以及地質(zhì)類或礦產(chǎn)資源類研究生使用。作者萬天豐是中國地質(zhì)大學(xué)（北京）教授。

書籍目錄

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
　……

章節(jié)摘錄

版權(quán)頁：插圖：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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