Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1007/s11631-013-0636-0 |
Deep-penetrating geochemistry of the Tuwu copper deposit, northwestern China | |
Wen Xueqin; Zhao Shanding; Zhang Hong | |
通讯作者 | Wen, XQ |
来源期刊 | ACTA GEOCHIMICA
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ISSN | 2096-0956 |
EISSN | 2365-7499 |
出版年 | 2013 |
卷号 | 32期号:3页码:303-312 |
英文摘要 | Desert terrains in northern China are covered by widespread regolith sediments which mask geochemical signals from ore bodies and are major obstacles to mineral exploration. There is a critical need to study the vertical distribution of elements in this regolith and to establish optimum sampling and analytical methods. The aim of this study is to understand the dispersion and variation of elements throughout the cover in a vertical profile. The results demonstrate that the main elements show a distribution pattern of enrichment in clay layers in the vertical profile, i.e., most elements tend to be enriched in the most upper part of the profile above the orebodies except for some elements like Cu, Ca and Ag. Meanwhile, both fine (-160 mesh) and coarse (+ 20 mesh) fraction samples from clay-rich horizons are favorable samples and selective leaching of the elements absorbed on clays or oxide coatings is effective for localizing buried deposits. The distribution of active Cu and Mo is quite different because chalcopyrite is weathered into Cu sulfate and CuCO3, and is precipitated in alkaline environments in a layer below close to the surface. Mo is soluble in the alkaline environment so it can penetrate the caliche layer and be enriched on the surface of soil enriched with weakly cemented clay. |
英文关键词 | desert regolith vertical variation buried ore-body mobile element: Tuwu copper deposit |
类型 | Article |
语种 | 英语 |
收录类别 | ESCI |
WOS记录号 | WOS:000218354500009 |
WOS关键词 | CONTINENTAL GROWTH ; MOBILE FORMS ; EXPLORATION ; OVERBURDEN ; EVOLUTION ; XINJIANG ; METALS |
WOS类目 | Geochemistry & Geophysics |
WOS研究方向 | Geochemistry & Geophysics |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/330400 |
作者单位 | [Wen Xueqin; Zhang Hong] Taiyuan Univ Technol, Sch Min Technol, Dept Geosci, Taiyuan 030024, Peoples R China; [Zhao Shanding] Changan Univ, Xian 710054, Peoples R China; [Zhao Shanding] CAGS, Key Lab Appl Geochem, Langfang 065000, Peoples R China |
推荐引用方式 GB/T 7714 | Wen Xueqin,Zhao Shanding,Zhang Hong. Deep-penetrating geochemistry of the Tuwu copper deposit, northwestern China[J],2013,32(3):303-312. |
APA | Wen Xueqin,Zhao Shanding,&Zhang Hong.(2013).Deep-penetrating geochemistry of the Tuwu copper deposit, northwestern China.ACTA GEOCHIMICA,32(3),303-312. |
MLA | Wen Xueqin,et al."Deep-penetrating geochemistry of the Tuwu copper deposit, northwestern China".ACTA GEOCHIMICA 32.3(2013):303-312. |
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