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Discovery of Middle Triassic radiolarian fauna from the Nan area along the Nan-Uttaradit suture zone, northern Thailand

机译:在泰国北部Nan-Uttaradit缝合带的Nan地区发现中三叠世放射虫动物区系

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摘要

A Middle Triassic radiolarian fauna is present in the siliceous rock section at the Nan area along the Nan-Uttaradit suture zone, northern Thailand. The radiolarian fauna is composed of Triassocampe deweveri, T. nishimurai, Annulotriassocampe campanilis, Cenosphaera igoi, and other species and corresponds to the Anisian (Middle Triassic) Triassocampe deweveri fauna reported from Japan, Hungary, Italy, Austria, Far East of Russia, and northern and eastern Thailand. More than fifteen radiolarian species belonging to eight genera are investigated. The radiolarian-bearing rocks were probably deposited in a pelagic environment within the Nan-Uttaradit back-arc basin between the Simao and Indochina blocks during Middle Triassic time. This suggests that the Nan-Uttaradit back-arc basin, the Palaeo-Tethys ocean and Panthalassa ocean were probably connected by seaways at this time and might have shared the same oceanic circulation system. Furthermore, the complete closure of the Nan-Uttaradit back-arc basin between the Simao and the Indochina blocks is thought to have occurred at least after the Middle Triassic.
机译:在泰国北部Nan-Uttaradit缝合带的Nan地区,硅质岩段中存在一个中三叠世放射虫动物群。放射虫动物群由Triassocampe deweveri,T。nishimurai,Annulotriassocampe campanilis,Cenosphaera igoi等物种组成,对应于日本,匈牙利,意大利,奥地利,俄罗斯远东和俄罗斯所报道的Anisian(中三叠纪)Triassocampe deweveri动物群。泰国北部和东部。调查了属于8个属的15种放射虫种类。含放射虫的岩石可能在中三叠世时期沉积在思茅和印度支那区块之间的南北程背弧盆地的中上层环境中。这表明,此时南-程逸背弧盆地,古特提斯洋和潘塔拉萨洋可能已通过海路相连,并且可能具有相同的海洋环流系统。此外,人们认为至少在中三叠纪之后才完全关闭了思茅与印度支那地块之间的南北陆背弧盆地。

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