西昆仑塔什库尔干马尔洋岩组的厘定及控矿意义
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摘要
塔什库尔干大型铁矿成矿带位于昆仑造山带西段,原岩恢复表明该区含铁岩系主要为一套双峰式火山岩-碎屑岩-碳酸盐岩建造组合,岩石普遍遭受绿片岩相变质和多期构造变形。本文报道了在老并一带变安山岩中获得的LA-ICP-MS锆石U-Pb同位素年龄值(603±10) Ma,并结合前人年龄数据,将原划古元古界布伦阔勒岩群的含铁岩系厘定为震旦系—寒武系纽芬兰统马尔洋岩组(Z?1m),其内发育典型的双峰式火山岩组合,证实了区内震旦纪—早寒武世仍处于拉张伸展背景,变质火山-沉积组合特征表明其形成于大陆边缘裂谷构造环境。含铁岩系典型的膏(钡)-铁建造很可能为新元古代晚期"Marinoan雪球"冰期后地球系统变化的火山-沉积响应。
The Taxkorgan large-scale iron metallogenic belt is located in the western part of Kunlun orogenic belt. Research on metamorphic rocks shows that the protolith of the iron-bearing strata is a assemblage of bimodal volcanic rocks-clastic rockscarbonate rocks formation. The strata have undergone widespread greenschist facies metamorphism and multi-superimposed deformation. The meta-andesite in Laobing area yielded an U-Pb ziron age of(603±10) Ma, suggesting that the eruption age of volcanic rocks is early Sinian. Combined with other age data available, the authors redefined the iron-bearing strata as"SinianCambrian Terreneuvian Maeryang Formation"(Z?1 m.), which doesn't belong to the previously defined "PaleoproterozoicBulunkuole Group". The formation of the bimodal volcanic rocks proved that there was an extensional tectonic event in Taxkorgan area from Sinian to early Cambrian. Discrimination of tectonic setting on the metamorphic volcano-sedimentary formation indicates that the iron-bearing strata were formed in the continental margin rift. The gypsum(Ba)-iron formation was the volcanosedimentary response to the changes of"Marinoan Snowball Earth"'system after late Neoproterozoic glacial event.
The Taxkorgan large-scale iron metallogenic belt is located in the western part of Kunlun orogenic belt. Research on metamorphic rocks shows that the protolith of the iron-bearing strata is a assemblage of bimodal volcanic rocks-clastic rockscarbonate rocks formation. The strata have undergone widespread greenschist facies metamorphism and multi-superimposed deformation. The meta-andesite in Laobing area yielded an U-Pb ziron age of(603±10) Ma, suggesting that the eruption age of volcanic rocks is early Sinian. Combined with other age data available, the authors redefined the iron-bearing strata as"SinianCambrian Terreneuvian Maeryang Formation"(Z?1 m.), which doesn't belong to the previously defined "PaleoproterozoicBulunkuole Group". The formation of the bimodal volcanic rocks proved that there was an extensional tectonic event in Taxkorgan area from Sinian to early Cambrian. Discrimination of tectonic setting on the metamorphic volcano-sedimentary formation indicates that the iron-bearing strata were formed in the continental margin rift. The gypsum(Ba)-iron formation was the volcanosedimentary response to the changes of"Marinoan Snowball Earth"'system after late Neoproterozoic glacial event.
引文
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