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首页> 外文期刊>Journal of Asian earth sciences >SHRIMP geochronology for the 1450 Ma Lakhna dyke swarm: Its implication for the presence of Eoarchaean crust in the Bastar Craton and 1450-517 Ma depositional age for Purana basin (Khariar), Eastern Indian Peninsula
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SHRIMP geochronology for the 1450 Ma Lakhna dyke swarm: Its implication for the presence of Eoarchaean crust in the Bastar Craton and 1450-517 Ma depositional age for Purana basin (Khariar), Eastern Indian Peninsula

机译:1450 Ma Lakhna堤防群的SHRIMP年代学:对印度东部半岛的Purana盆地(Khariar)的Bastar Craton和1450-517 Ma沉积时代存在太古宙地壳的影响

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摘要

Zircon U-Pb ages of the Mesoproterozoic dyke swarms (Lakhna dyke swarm) at the interface between the Eastern Chats Mobile Belt and Bastar Craton of the Indian Peninsula are reported here to decipher the tectonic evolution of the region. The dyke swarm, which is dominantly N-S in orientation, has intruded the Bastar Craton at ca. 1450 Ma. The dykes vary in composition from dolerite to trachyte and rhyolite and have been emplaced in a continental anorogenic setting. The above age puts a tower time constraint on the sedimentary sequences of the Purana basin (Khariar basin) that have been deposited unconform-ably over the Bastar Craton. The shale member of the Khariar basin shows evidence of synsedimentary shearing suggesting that the sedimentation probably continued up to 517 Ma, the age of shearing and overthrusting of the granulite nappes of the Eastern Chats Mobile Belt on the Craton. Further, the compression accompanying thrusting of the nappes, uplifted the Purana basins during inversion.
机译:据报道,在印度东部半岛东部流动带和印度半岛的巴斯塔尔·克拉通之间的交界的中元古代堤群(拉赫纳堤群)的锆石U-Pb年龄可用来解释该地区的构造演化。堤坝群以N-S为主,入侵了约25英尺的Bastar Craton。 1450年。脉石的组成各不相同,从白云石到松散粒状岩和流纹岩,都被放置在大陆性厌食环境中。以上年龄对Purana盆地(Khariar盆地)的沉积序列施加了塔时间限制,这些沉积序列不整合地沉积在Bastar Craton上。 Khariar盆地的页岩段显示了同沉积剪切作用的证据,这表明沉积可能持续到517 Ma,这是克拉顿东部Chats Mobile Belt的粒状尿布剪切和推覆的年龄。此外,在逆转过程中,伴随着尿布推挤的压缩使Purana盆地抬升。

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