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Geology, Geochemistry and Origin of the Hongshan Porphyry-Cryptoexplosive Breccia Type Copper Deposit in Huichang County, Jiangxi Prvince 被引量:6
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作者 ZHOU Jiyuan CUI Bingfang CHEN Shizhong 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 1999年第1期19-29,共11页
The Hongshan porphyry-cryptoexplosive breccia type copper deposit occurs in a metamorphic rock series of the Mesoproterozoic Zhongcun Group. Orebodies are distributed inside and outside porphyry-cryptoexplosive brecci... The Hongshan porphyry-cryptoexplosive breccia type copper deposit occurs in a metamorphic rock series of the Mesoproterozoic Zhongcun Group. Orebodies are distributed inside and outside porphyry-cryptoexplosive breccia pipes. The deposit involves five ore-forming types, i.e the porphyry type, cryptoexplosive breccia type, contact-zone veinlet-disseminated type, in-pipe fracture-zone filling-replacement type and out-of-pipe fracture-zone filling-replacement type, forming an ore-forming system of “five ore-forming types within a single rock body”. Fluid inclusion and isotope geochemical studies indicate the following: S, Pb, O and Sr were derived from the lower crust, Nd was derived from the continental crust or depleted mantle and rare earth elements (REE) and trace elements have the crustal source characters; fluids consist dominantly of formation water, metamorphic water and ***meteoric water with a part of magmatic mater, heat came from porphyry while the latter originated from partial melting caused by shear heating in the lower crust and upper mantle. According to its origin the deposit is classified as the hypabyssal and near-surface, meso- and hypothermal copper deposit associated with the late Yanshanian porphyry-cryptoexplosive breccia. 展开更多
关键词 PORPHYRY cryptoexplosive breccia copper deposit Hongshan Huichand JIANGXI
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Discovery of Liquid Cryptoexplosive Breccia in the Pulang Porphyry Copper Deposit of Yunnan Province and its Prospecting Significance
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作者 SHI Hongzhao FAN Wenyu +2 位作者 WANG Xianfeng TAN Gengli LIU Shusheng 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2015年第4期1421-1422,共2页
The Pulang porphyry copper deposit,located in the Gezan tectonic-magmatic arc and south of the Yidun island arc,southwest of Sanjiang metallogenic belt in Yunnan province,is a super-large porphyry copper deposit.
关键词 Discovery of Liquid cryptoexplosive Breccia in the Pulang Porphyry Copper Deposit of Yunnan Province and its Prospecting Significance ROCK
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Geology and Genesis of the Superlarge Jinchang Gold Deposit,NE China
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作者 JIA Guozhi CHEN Jinrong +5 位作者 YANG Zhaoguang BIAN Hongye WANG Yangzhong LIANG Haijun JIN Tonghe LI Zhenhui 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2008年第4期750-761,共12页
The superlarge Jinchang gold deposit is located in the joint area between the Taipingling uplift and the Laoheishan depression of the Xingkai Block in both eastern Jilin and eastern Heilongjiang Province. Wall rocks o... The superlarge Jinchang gold deposit is located in the joint area between the Taipingling uplift and the Laoheishan depression of the Xingkai Block in both eastern Jilin and eastern Heilongjiang Province. Wall rocks of the gold deposits are the Neoproterozoic Huangsong Group of metamorphic rocks. Yanshanian magmatism in this region can be divided into 5 phases, the diorite, the graphic granite, the granite, the granite porphyry and the diorite porphyrite, which resulted in the magmatic domes and cryptoexplosive breecia chimney followed by large-scale hydrothermal alteration. Gold mineralization is closely related to the fourth and fifth phase of magmatism. According to the occurrences, gold ores can be subdivided into auriferous pyritized quartz vein, auriferous quartz-pyrite vein, auriferous polymetailic sulfide quartz vein and auriferous pyritized calcite vein. The ages of the gold deposit are ranging from 122.53 to 119.40 Ma. The ore bodies were controlled by a uniform tectono-magmatic hydrothermal alteration system that the ore-forming materials were deep derived from and the ore-forming fluids were dominated by magmatic waters with addition of some atmospheric water in the later phase of mineralization. Gold mineralization took place in an environment of medium to high temperatures and medium pressures. Ore-forming fluids were the K^+-Na^+-Ca^2+-Cl^--SO4^2- type and characterized by medium salinity or a slightly higher, weak alkaline and weak reductive. Au in the ore-forming fluids was transported as complexes of [Au (HS)2]^-, [AuCl2]^-, [Au(CO2)]^- and [Au(HCO3)2]^-. Along with the decline of temperatures and pressures, the ore-forming fluids varied from acidic to weak acidic and then to weak alkaline, which resulted in the dissociation of the complex and finally the precipitation of the gold. 展开更多
关键词 magmatic dome cryptoexplosive breccia pipe ring and radial faults gold deposit superlarge JINCHANG Taipingling Heilongjiang
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