| 新疆康古尔断裂带东段的地球化学特征 |
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| 引用本文： | 白云来. 新疆康古尔断裂带东段的地球化学特征[J]. 新疆地质, 1991, 0(3) |
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| 作者姓名： | 白云来 |
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| 作者单位： | 新疆维吾尔自治区地质矿产局第六地质大队 |
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| 摘 要： | 新疆康古尔断裂带东段(土墩—黄山)的地球化学异常规模大,元素组合为铜、钴、镍铁、钒、钛、铬、钇、锆、铌、金、银等.从聚类分析、因子分析结果及镍、铬、钴、钛、钒累乘等值线图表明,康古尔断裂两侧地球化学系统明显不同,是性质不同的两个壳块.断裂带存在有“榴辉岩化地壳”.康古尔断裂可能是哈萨克斯坦—准噶尔古板块与塔里木古板块间的分界线.
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| 关 键 词： | 康古尔断裂 元素组合 榴辉岩化地壳 地球化学系统 |
GEOCHEMlCAL CHARACTERISTICS OF EASTERN KANGGUR FAULT, XINJIANG |
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| Bai Yunlai. GEOCHEMlCAL CHARACTERISTICS OF EASTERN KANGGUR FAULT, XINJIANG[J]. Xinjiang Geology, 1991, 0(3) |
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| Authors: | Bai Yunlai |
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| Abstract: | Geochemical characteristics of eastern Kanggur fault in Tudun-Huangshan section are described in this paper. Anomalies are larger in scale on the faultzone. The elemental association includes Cu, Co, Ni, Fe, Cr, V, Ti, Y, Zr, Nb,Au, AS etc. The Cluster analysis, factor analysis and Ni, Cr, Co, Ti.V multiplicative isogram show that the Geochemical system and the nature of crustal blocks are obviously different on both sides of the fault. "Eclogitization crust" may exist in the fault belt. The author considers that kanggur fault may be the boundary of the Kazakhstan-Junggar and Tarim paleoplate. |
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| Keywords: | Kanggur fault elemental association eclogitization crust geochemical system |
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