首页> 外文会议>International Symposium of Geological and Mineragenic Correlation in Contiguous Regions of China, Russia and Mongolia; 20031008-11; Changchun(CN) >Geological Position and Conditions of the Formation of Larginsk Deposit of Magnesites, Eastern Zabaikal
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Geological Position and Conditions of the Formation of Larginsk Deposit of Magnesites, Eastern Zabaikal

机译:扎拜卡尔东部镁质岩拉金斯克矿床的地质位置和形成条件

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摘要

Larguinsk deposit is located in Larguinsko-Kaktolguinsk magnesite region (LKMR) to the south from West-Stanovoy structure-formation zone in Mongolian-Zabaikal folded region. At the northern part the Larguinsk deposit side with Mogolian-Okhotsk deep fault. The rock with the high content of the magnesia of the Shilkinsk basite-ultrabasite belt is taken out on the surface along this deep fault. As a result of the following destruction this rock had been brought to the nearby shallow lagoons. Probably it was the resource of the magnesite formation.
机译:Larguinsk矿床位于蒙古-Zabaikal折叠区西-Stanovoy结构形成区以南的Larguinsko-Kaktolguinsk菱镁矿区(LKMR)。在北部的拉尔金斯克矿床一侧,伴有蒙古-鄂霍次克深断层。沿着该深层断层带出了希尔金斯克州贝氏体-超贝氏体带氧化镁含量高的岩石。由于随后的破坏,该岩石被带到附近的浅泻湖。可能是菱镁矿形成的资源。

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