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在新疆东昆仑木孜塔格蛇绿岩的硅岩中发现了早石炭世杜内晚期的EarlyAlbaillella indensis Zone放射虫组合,从而可将该蛇绿岩的年龄上限确定为早石炭世。放射虫组合、硅岩沉积特征以及同埋藏群的海绵骨针类都指示被研究的区域在早石炭世杜内晚期或甚至更早的时期已处于半深海至深海环境。该蛇绿岩代表的消失洋盆与可可西里和祁漫塔格等地区的古洋盆共同构成了青藏高原北部早石炭世古特提斯多岛海的一部分,同时说明早石炭世青藏高原北部陆壳的裂解是沿多处进行的。
Early Early Stage Carboniferous EarlyAlbaillella indensis Zone radiolarian assemblage was found in the silicate rocks of the Muztag Tomb of the East Kunlun Mountains in the eastern Kunlun Mountains so that the upper age limit of the ophiolite can be identified as Early Carboniferous. Radiolarian assemblages, sedimentary features of silicon rocks, and sponge spicules of the same burial group all indicated that the area under study was in the semi-deep ocean to deep-sea environment during the Late Carboniferous Dunes or even earlier periods. The disappearing ocean basin represented by this ophiolite, together with the ancient oceanic basins such as Hoh Xil and Qimantag, form part of the Early Epikote of the ancient Tethys Island in the northern part of the Qinghai-Tibet Plateau. Meanwhile, the continental crust in the northern part of the Early Carboniferous Tibetan Plateau The cleavage is carried out in many places.