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引用本文:欧阳永棚,饶建锋,廖绍平,何细荣,胡青华,魏锦,杨明桂. 赣东北朱溪矿集区构造控岩-控矿特征[J]. 中国地质, 2019, 46(4): 878-893.
OUYANG Yongpeng,RAO Jianfeng,LIAO Shaoping,HE Xirong,HU Qinghua,WEI Jin,YANG Minggui. Rock-and ore-controlling structure in the Zhuxi ore concentration area in the northeastern Jiangxi Province[J]. Geology in China, 2019, 46(4): 878-893(in Chinese with English abstract).
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赣东北朱溪矿集区构造控岩-控矿特征
欧阳永棚1, 饶建锋1, 廖绍平2, 何细荣1, 胡青华3, 魏锦1, 杨明桂3
1.江西省地质矿产勘查开发局九一二大队, 江西 鹰潭 335001;2.江西省地质矿产勘查开发局物化探大队, 江西 南昌 330002;3.江西省地质矿产勘查开发局, 江西 南昌 330002
摘要:
赣东北朱溪为钦杭成矿带新发现的重要钨铜多金属矿集区,位于钦杭结合带萍(乡)乐(平)坳陷带东部逆冲推覆抬升地段。朱溪矿集区燕山期受逆冲推覆构造影响,形成由新元古界变质基底与上古生界-中生界沉积盖层组成的构造岩片堆叠构造;具有逆冲推覆深断裂带控岩-控矿、碳酸盐岩构造岩片赋矿、燕山晚期浅层对冲构造破矿的构造背景;发育有燕山早期I型花岗闪长(斑)岩钼铜和S型花岗岩钨铜两个岩浆岩成矿系列,在空间上形成张家坞—月形与塔前—朱溪两个矿田、张家坞—毛家园和塔前—朱溪上下两个成岩台阶,下成矿台阶朱溪巨大钨铜矿床的发现打开了钦杭成矿带坳陷区“深地”找矿的一扇窗户。
关键词:  逆冲推覆构造带  I+S型岩浆成矿系列  多台阶成矿  朱溪矿集区
DOI:10.12029/gc20190417
分类号:P548
基金项目:中国地质调查局项目(121201103000150017、12120113065300、DD20160346、DD20160082、DD20190012)和江西省地质矿产勘查开发局项目(赣地矿字[2017]78号)联合资助。
Rock-and ore-controlling structure in the Zhuxi ore concentration area in the northeastern Jiangxi Province
OUYANG Yongpeng1, RAO Jianfeng1, LIAO Shaoping2, HE Xirong1, HU Qinghua3, WEI Jin1, YANG Minggui3
1.No. 912 Geological Surveying Party, Jiangxi Bureau of Geology and Mineral Exploration and Development, Yingtan 335001, Jiangxi, China;2.Geophysical & Geochemical Exploration Party, Jiangxi Bureau of Geology and Mineral Exploration and Development, Nanchang 330002, Jiangxi, China;3.Jiangxi Bureau of Geology and Mineral Exploration and Development, Nanchang 330002, Jiangxi, China
Abstract:
Zhuxi is a newly discovered W-Cu ore concentration area in the Qinzhou-Hangzhou metallogenic belt, northeastern Jiangxi Province. It is situated in the lifting area of the thrust nappe structure in eastern Pingxiang-Leping depression, Qinzhou-Hangzhou orogenic juncture belt. Due to the Yanshanian thrust nappe tectonic events, the Zhuxi ore concentration area is dominated by Neoproterozoic metamorphic basement and Upper Paleozoic -Mesozoic tectonic slices. The ore deposits in this region are controlled by thrust nappe deep faults, hosted in carbonatite tectonic slices, and transformed by superficial hedge structures. The early Yanshanian metallogenesis can be subdivided into two groups:(1) Mo -Cu metallogenic system related to the I -type (porphyritic) granodiorite; (2) W-Cu metallogenic system related to the S-type granite. The Zhuxi area is characterized by two orefields (Taqian-Zhuxi and Zhangjiawu-Yuexing) and two magmatic steps (Maojiayuan-Zhangjiawu and Zhuxi-Taqian). The discovery of the Zhuxi giant W-Cu deposit opens a window for the deep mineral exploration in the geotectogene of the Qinzhou-Hangzhou metallogenic belt.
Key words:  thrust nappe structure  I-and S-type magma-mineralization series  multi-step mineralization  Zhuxi ore concentration area