| 东秦岭沉积建造演化与成矿 |
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| 关键词:sedimentary formation metallogenic assemblage tectonic evolution paleocontinental margin East Qinling Mountain |
| 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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| 摘要: |
| The Development of Sedimentary Buildups and Mineralization in the Eastern Qinling Mountain |
| 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. |
| ZHANG Zheng-wei,YANG Huai-zhou,ZHU Bing-quan.2003.The Development of Sedimentary Buildups and Mineralization in the Eastern Qinling Mountain[J].Acta Geoscientica Sinica,24(4):293-298. |
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