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首页> 外文期刊>Earth-Science Reviews: The International Geological Journal Bridging the Gap between Research Articles and Textbooks >Post-cratonization deformation processes and tectonic evolution of the North China Craton
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Post-cratonization deformation processes and tectonic evolution of the North China Craton

机译：北北京克拉顿后裂缝后变形过程与构造演化

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The timing of events during the tectonic evolution of the North China Craton (NCC) and the east China region is debated. Extension, compression, transpression, and shearing occurred throughout the NCC since similar to 320 Ma. These main structural stages and the temporal evolution of the structural framework and kinematics are summarized. We present here data from multiple structural and magmatic stages related to temporally varying kinematics and deformation mechanisms during the evolution of the post-cratonization of the NCC. The timing of each stage is constrained using isotopic dating, along with the timing of magmatic intrusion, dyke intrusion, and basin formation associated with tectonic transformation of the NCC. Age data indicate distinct structural and magmatic stages at similar to 1600-1500, 1300-1100, 445-315, 270-200, 170-155, 130-110, 75-65, and 25-20 Ma, relating to basin formation and continental uplift or collapse. These stages define the tectonic evolution and structural transformation of the NCC and associated de-rooting, reactivation, reworking, and orogenic growth. The tectonic setting and movement direction of adjacent plates changed multiple times during the various stages. The stages are as follows: separation of the NCC from the Gondwana supercontinent and northwards drift; formation of the Central Asian orogenic belt (CAOB) and northwards subduction of the Yangtze plate, resulting in closure of the Qinling Ocean; the rapid initial formation of the western Pacific plate and subsequent subduction; and final closure of the Mongol-Okhotsk Ocean, combined with closure of the Bangong-Nujiang Suture Zone and southwards movement of the Siberian continent, as well as thinning of the North China cratonic lithosphere. Moreover, temporal and spatial changes in deformation, magmatism, and basin formation, as well as kinematic and mechanical transformations, occurred in response to the changing tectonic setting and movement direction of surrounding plates
机译：辩论了华北克拉顿（NCC）和华东地区构造演变期间的事件时间。在整个NCC中发生延伸，压缩，变形和剪切，因为类似于320 mA。总结了这些主要结构阶段和结构框架和运动学的时间演变。我们在这里介绍来自多个结构和岩浆阶段的数据，与在NCC的裂缝后裂缝后的演变期间与时间上变化的运动学和变形机制相关。每个阶段的定时使用同位素约会约束，以及与NCC的构造变换相关的岩石侵入，堤防侵入和盆地形成的时序。年龄数据表示与1600-1500,1300-1100,445-315,270-200,170-155,130-200,75-65和25-20 mA相似的不同的结构和岩浆阶段，与盆地形成和25-20 mA类似，大陆隆起或崩溃。这些阶段定义了NCC的构造演化和结构转化，以及相关的去生根，再活化，再加工和造口生长。相邻板的构造设定和移动方向在各个阶段期间多次变化。阶段如下：将NCC与北北面和北漂移的分离;形成中亚造山带（Caob）和北部的长江北部的形成，导致秦岭闭合;西太平洋板的快速初始形成和随后的俯冲;并最终关闭了蒙古 - 鄂霍茨克海洋，结合了邦贡 - 怒江缝合区和西伯利亚大陆向南运动的关闭，以及华北克拉廷岩石圈的减薄。此外，响应于改变构造设定和周围板的移动方向而发生变形，岩浆和盆地形成以及运动和机械变换的时间和空间变化，以及运动和机械变换

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