| 东秦岭沉积建造演化与成矿 |
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| 引用本文：张正伟,杨怀洲,朱炳泉.2003.东秦岭沉积建造演化与成矿[J].地球学报,24(4):293-298. |
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| 基金项目:国家自然科学基金(编号40072033)；中国科学院知识创新工程重要方向项目(KZCX2-SW-125)；国家重点基础研究发展规划项目(编号:G1999043213) |
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| 中文摘要:在华北古大陆南缘，以控制不同构造单元的断裂为界，构造格局自北而南划分如下：古大陆边缘的基底与盖层单元(华—熊陆缘带)，宽坪群构造单元，二郎坪群构造单元，北秦岭(秦岭群)构造单元和南秦岭(刘岭群)构造单元。据陆缘构造发展阶段的沉积建造和岩石组合控矿因素，划分该区沉积建造演化阶段：①前长城纪陆核活动性边缘沉积建造；②中、新元古代被动大陆边缘沉积建造；③早加里东期构造体制转换期演化阶段；④古生代活动大陆边缘沉积建造；⑤中生代陆内碰撞演化阶段。从时间与空间角度，分别研究了不同构造演化阶段的成矿问题。 |
| 中文关键词:沉积建造 矿床 构造演化 古陆边缘 东秦岭 |
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| The Development of Sedimentary Buildups and Mineralization in the Eastern Qinling Mountain |
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| Abstract:According to tectonic characteristics of the study area on the southern margin of North China paleocontinent, the geotec-tonic framework of the area could be divided into five units:(1)the Huashan-Xong'er Mountains continental margin belt;(2)the Kuan-ping Late Proterozoic accretion belt of the paleocontinent;(3)the Erlangping margin basin zone;(4)the Qinling dispersion type island arc terrain; (5)the sedimentary basins of Nanqinling zone. In the light of the evolutionary stages of the sedimentary formation as well as metallogenesis, it can be classified into:(1)the sedimentary formation in the active southern margin of the pre-Mesoproterozoic North China Paleocontinent;(2)the sedimentary formation in the Middle-Late Proterozoic inactive continent margin; (3)the sedimentary formation in the early Paleozoic converse type continent margin;(4)the sedimentary formation in the Paleozoic active margin;(5)the phase of Mesozoic collision. |
| keywords:sedimentary formation metallogenic assemblage tectonic evolution paleocontinental margin East Qinling Mountain |
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