中国大陆中东部早白垩世伸展穹隆构造与多金属成矿
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摘要
中国中东部晚中生代伸展构造十分显著,表现为大量发育伸展成因的穹隆构造和地堑-半地堑盆地。对这些伸展穹隆系统的分析、归纳和总结,将中国中东部早白垩世伸展构造发育区划分为:华北西部带、华北东部带、华北南缘及秦岭-大别带和华南内陆带。区域上,这些伸展构造均具有NW-SE的伸展方向,与蒙古及俄罗斯泛贝加尔-鄂霍茨克带一同构成了全球最大的大陆岩石圈伸展地区。这些伸展构造使中下地壳的结构发生了强烈的改造,并使一些中深变质岩出露到地表。在华北地区,这期伸展构造具有对称性的特点,即华北西部带向NW拆离,相关的岩石变形大体上具有上部向SE的运动学特征;而华北东部带向SE拆离,伸展穹隆主体具有上部向NW的运动学特征。同位素年代学研究揭示伸展穹隆形成的峰期时间十分相近:集中在130～120 Ma之间。高大地热流值背景所代表的岩石圈伸展环境,与地球化学研究结果所揭示的大规模壳-幔作用具有非常好的耦合性,并诱发了我国中东部晚中生代岩浆-热液活动及其相关大规模的成矿作用。中东部的成矿带与同时代的伸展构造具有很好的吻合性。
The Late Mesozoic extensional tectonics was quite significant on the central and eastern China. This extensional tectonics was expressed by the metamorphic core complexes(MCC), syn-tectonic magmatic domes or syn-tectonic plutons, rolling-hinge structures, and vast graben/half graben basins. According to ours and previous research work, four extension tectonic regimes have been determined: the western part of the North China domain, the eastern part of the North China domain, the southern margin of the North China and Qinling-Dabie domain, the interior of the South China Block domain. The direction of this Early Cretaceous extension tectonic was NW-SE in these four domains. As the largest crustal scale extensional tectonic in the world, this extreme extensional event exhumed the different levels of the crust rocks to the surface along detachment faults. This exhumation process destructed the crust of the eastern part of the North China Craton. In North China, the extensional tectonic is characterized by symmetry.Related geochronological works on the detachment faults constrain the activity period of the Early Cretaceous(ca. 130–120 Ma). The lithospheric extension represented by the high geothermal flow corresponding well to the large-scale crust-mantle reaction revealed by the geochemical work. This interaction induced extensive magmatic-hydrothermal activities and related massive polymetallic mineralization in the central and eastern China.
The Late Mesozoic extensional tectonics was quite significant on the central and eastern China. This extensional tectonics was expressed by the metamorphic core complexes(MCC), syn-tectonic magmatic domes or syn-tectonic plutons, rolling-hinge structures, and vast graben/half graben basins. According to ours and previous research work, four extension tectonic regimes have been determined: the western part of the North China domain, the eastern part of the North China domain, the southern margin of the North China and Qinling-Dabie domain, the interior of the South China Block domain. The direction of this Early Cretaceous extension tectonic was NW-SE in these four domains. As the largest crustal scale extensional tectonic in the world, this extreme extensional event exhumed the different levels of the crust rocks to the surface along detachment faults. This exhumation process destructed the crust of the eastern part of the North China Craton. In North China, the extensional tectonic is characterized by symmetry.Related geochronological works on the detachment faults constrain the activity period of the Early Cretaceous(ca. 130–120 Ma). The lithospheric extension represented by the high geothermal flow corresponding well to the large-scale crust-mantle reaction revealed by the geochemical work. This interaction induced extensive magmatic-hydrothermal activities and related massive polymetallic mineralization in the central and eastern China.
引文
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