剥离断层—50矿床的主控因素
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P613


PEEL THRUSTS--A DOMINANT ORE--CONTROLLING FACTOR OF DEPOSIT NO. 50
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    摘要:

    燕山晚期的拉张构造环境,在深断裂带或裂陷带两侧形成了各种不同层次的拆离滑脱,包括剥离断层。信江裂陷带南侧的F15剥离断层(系统)控制了50矿床的矿质来源,矿质沉淀及矿体定位。该断层是控矿的主导因素。文中还讨论了剥离断层的找矿意义。

    Abstract:

    The Late Yanshanian extensional environment gave rise to detachments,including peel thrusts, at various tectonic levels on both sides of the deep faultbelt or rift belt. F_(15) peel thrust (system) at the southern side of the Xinjiangrift belt is a dominant ore-controlling factor of deposit No. 50. It is beleived tocontroll the source of ore substances and their precipitation and siting of theorebodies. Besides, the paper also discusses the significance of peel thrusts inmineral prospecting.

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张万良.1994.剥离断层—50矿床的主控因素[J].地质论评,40(6):502-507,[DOI].
Zhang Wanliang.1994. PEEL THRUSTS--A DOMINANT ORE--CONTROLLING FACTOR OF DEPOSIT NO. 50[J]. Geological Review,40(6):502-507.

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