首页> 外文期刊>Journal of the Geological Society of India >Ooids in Sillakkudi Formation of Ariyalur Group of Tiruchirapalli Cretaceous, Tamil Nadu: Implications for Origin and Depositional Environment
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Ooids in Sillakkudi Formation of Ariyalur Group of Tiruchirapalli Cretaceous, Tamil Nadu: Implications for Origin and Depositional Environment

机译:泰米尔纳德邦Tiruchirapalli白垩纪Ariyalur组Sillakkudi组的Ooids:对成因和沉积环境的影响

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摘要

An ooid-rich limestone band of Sillakkudi Formation is encountered in a well section near Ariyalur. The ooids are believed to be deposited in a marine regime. They contain berthierine as the major mineral and haematite, siderite and quartz as minor minerals. They exhibit alternate rings of berthierine and haematite which shows that these minerals were developed under changing physico-chemical conditions. In the present paper, the petrographical characters, mineralogy, origin and depositional environment of the ooids are discussed.
机译:在Ariyalur附近的一个井段遇到了Sillakkudi组的富含卵石的石灰岩带。人们认为,该类卵磷脂是在海洋中沉积的。它们含有黄柏素作为主要矿物质,赤铁矿,菱铁矿和石英为次要矿物质。它们展示了黄连和赤铁矿的交替环,表明这些矿物质是在不断变化的理化条件下形成的。本文讨论了类风岩的岩石学特征,矿物学,成因和沉积环境。

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