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Geochemistry of the Cenozoic Potassic Volcanic Rocks in the west kunlun mountains and Constraints on Their Sources

Acta Geologica Sinica(English Edition) 2004年第4期78卷 912-920页

作者： ZHANGZhaochong XIAOXuchang WANGJun WANGYong LUOZhaohua InstituteofGeology ChineseAcademyofGeologicalSciencesBeijing100037 InstituteofGeology ChineseAcademyofGeologicalSciencesBeijing100037／／ChinaUniversityofGeosciencesBeijing100087 ChinaUniversityofGeosciences Beijing100087

The geochemical characteristics of the Cenozoic volcanic rocks from the north Pulu, east Pulu and Dahongliutan regions in the west kunlun mountains are somewhat similar as a whole. However, the volcanic rocks from the Dahongliutan region in the south belt are geochemically distinguished from those in the Pulu region (including the north and east Pulu) of the north belt. The volcanic rocks of the Dahongliutan region are characterized by relatively low TiO2 abundance, but more enrichment in alkali, much more enrichment in light rare earth elements and large ion lithosphile elements than those from the Pulu region. Compared with the Pulu region, volcanic rocks from the Dahongliutan region have relatively low 87Sr/86Sr ratios, and high εNd, 207Pb/204Pb and 208Pb/204Pb. Their trace elements and isotopic data suggest that they were derived from lithospheric mantle, consisting of biotite- and hornblende-bearing garnet lherzolite, which had undertaken metasomatism and enrichment. On the primitive mantle-normalized patterns, they display remarkably negative Nb and Ta anomalies, indicating the presence of early-stage subducted oceanic crust. The metasomatism and enrichment resulted from the fluid released from the crustal materials enclosed in the source region in response to the uplift of asthenospheric mantle. Based on the previous experiments it can be inferred that the thickness of the lithosphere ranges from 75 to 100 km prior to the generation of the magmas. However, the south belt differs from the north one by its thicker lithosphere and lower degree of partial melting. The different thickness of the lithosphere gives rise to corresponding variation of the degree of crustal contamination. The volcanic rocks in the south belt are much more influenced by crustal contamination. In view of the tectonic setting, the generation of potassic magmas is linked with the uplift of asthenosphere resulted from large-scale thinning of the lithosphere after the collision of Indian and

关键词： potassic magma lithospheric mantle asthenospheric mantle metasomatism west kunlun mountains

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Ore-forming Conditions and Prospecting in the west kunlun Area,Xinjiang, China

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Acta Geologica Sinica(English Edition) 2004年第2期78卷 345-351页

作者： DONGYongguan GUOKunyi XIAOHuiliang ZHANGChuanlin ZHAOYu NanjingInstituteofGeologyandMineralResources NanjingJiangsu210016 FacultyofEarthSciences ChinaUniversityofGeosciencesWuhanHubei430074／／NanjingInstituteofGeologyandMineralResourcesNanjingJiangsu210016

The west kunlun ore-forming belt is located between the northwestern Qinghai-Tibet Plateau and southwestern Tarim Basin. It situated between the Paleo-Asian Tectonic Domain and Tethyan Tectonic Domain. It is an important component of the giant tectonic belt in central China (the kunlun-Qilian-Qinling Tectonic Belt or the Central Orogenic Belt). Many known ore-forming belts such as the kunlun-Qilian Qinling ore-forming zone, Sanjiang (or Three river) ore-forming zone, Central Asian ore-forming zone, etc. pass through the west kunlun area. Three ore-forming zones and seven ore-forming subzones were classified, and eighteen mineralization areas were marked. It is indicated that the west kunlun area is one of the most favorable region for finding out large and superlarge ore deposits.

关键词： ore-forming conditions mineralization collecting area orogenic zone west kunlun mountains

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