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Huizhou Movement and its significance in Pearl River Mouth Basin, China

机译：惠州运动及其在中国珠江口盆地的意义及其意义

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AbstractThe Huizhou Movement refers to the Middle Eocene tectonic transition from the early to the late Wenchang Rifting stage (about 43 Ma ago) in the Pearl River Mouth Basin. Based on seismic reflection, drilling, logging and geological data, fault characteristic analysis, denudation thickness recovery, magmatism statistics, regional tectonic dynamics comparison and other methods are used to reveal the characteristics, properties and dynamic mechanism of the Huizhou Movement. The Huizhou Movement mainly shows the North-South transition of rifting and the migration along the faults, basement uplift, magmatic diapir and stratigraphic denudation. It is believed that the Huizhou Movement is a comprehensive reflection of plate interaction and lithospheric thinning process in the Pearl River Mouth Basin, which is closely related to the transition of lithosphere from initial rifting to rapid thinning, the India-Eurasia hard collision and the change of subduction direction of the Pacific plate. The Huizhou Movement has significant influence and control on the Paleogene hydrocarbon-generating sags and the development of hydrocarbon source rocks, sedimentary system and deep high-quality reservoir, hydrocarbon migration and accumulation in the Pearl River Mouth Basin.
机译：摘要惠州的运动是指从早期到后期的中间世文构造过渡阶段（约43mA前）在珠江口盆地。基于地震反射，钻探，测井和地质数据，故障特征分析，剥蚀厚度回收，岩浆统计，区域构造动力学比较等方法用于揭示惠州运动的特点，特性和动态机制。惠州运动主要展示了沿北方河流的转型和沿着故障的迁移，地下室隆起，岩浆王冠和地层剥落。据信，惠州运动是珠江口盆地板相互作用和岩石薄薄稀土过程的全面反映，与岩石圈的过渡到初步散步到快速变薄，印度 - 欧亚人的艰苦碰撞和变化密切相关太平洋板的划分方向。徽州运动对古酸烃凹陷和碳氢化合物源岩，沉积体系和深层高质量水库，珠江口盆地的碳氢化合物迁移和积累产生重大影响和控制。

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