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Late Cretaceous (Santonian-Maastrichtian) integrated Coccolith-Globotruncanid biostratigraphy of pelagic Limestones from the accretionary prism of Manipur, Northeastern India

机译:来自印度东北马尼普尔邦增生棱镜的晚白垩世(桑托尼亚-马斯特里赫特)整合的上层石灰石的Coccolith-Globotruncanid生物地层学

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摘要

Employing special preparation techniques, a rich and moderately preserved assemblage of planktonic foraminifera and coccoliths is documented from pelagic limestones of Melange Zone of Manipur ophiolite belt around Ukhrul area in northeastern India. Integrated biostratigraphy of five exotic limestone blocks encompassing a Late Santonian/Early Campanian to Late Maastrichtian time Slice is established; the low-latitude calcareous plankton zones of deep-sea facies identified in such a convergent plate margin terrain, are Correlated with published new biostratigraphic, geomagnetic and absolute time scale data. Initial rifting and birth of the Indo-Myanmar Ocean took place prior to Latest Santonian/Earliest Campanian and suturing was initiated by Latest Maastrichtian, as suggested by our Study.
机译:印度东北部Ukhrul地区Manipur蛇绿岩带的Melange带的浮游石灰岩中采用特殊的制备技术,记录了丰富而保存完好的浮游有孔虫和可可石的组合。建立了五个异质石灰岩块的综合生物地层学,包括晚桑顿时期/坎帕尼亚晚期至马斯特里赫特晚期时间切片;在这种收敛的板块边缘地形中识别出的深海相的低纬度钙质浮游生物带,与已发表的新生物地层,地磁和绝对时标数据相关。根据我们的研究,印度洋的最初裂谷和生出发生在最新的桑顿时期/最早的Campanian时期,缝合工作是由最新的Maastrichtian发起的。

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