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首页> 外文会议>Mineral Deposit Research: Meeting the Global Challenge >Tectonic domino effect and crust-mantle reaction in auriferous belt at eastern margin of Kiamusze massif-Hegang upheaval as the example
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Tectonic domino effect and crust-mantle reaction in auriferous belt at eastern margin of Kiamusze massif-Hegang upheaval as the example

机译：以Kiamusze断层-鹤岗隆起东缘的金耳带的构造多米诺骨效应和地幔幔反应为例

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摘要

Auriferous belt in eastern margin of Kiamusze massif is controlled by strike-slip fault belt and deep fluid. Transfer between Crust-Mantle reaction and dynamic system is the basic dynamic guarantee of activation to transportation to congregation to mineralization, transfer of tectonic stress field was its important manifestation. Activity of Peony river lithosphere fault cut mantle occurred anatectic process. This process activated and transferred the mineralized material became main drive of them. The process was one of the roots that lithogenesis and mineralization occurred. Fluid in mantle became ore-bearing fluid by crust-mantel reaction, which provided mineral source for fluid mineralization, and transfer to higher stratohorizon through deep fault. The fluid mineralized by deposition when the physical-chemical condition changed. Auriferous belt at eastern margin of Kiamusze massif is controlled by deep rupture,depositions are correlative. The auriferous belt's mineralization finished under same tectonic stress system. N-N-E and N-W-W correlated with it directional rupture and Hypabyssal-Superhypabyssal rock mass are the directions that ore-search for the future.
机译：Kiamusze断层东缘的金耳带是由走滑断层带和深部流体控制的。地幔幔反应与动力系统之间的转移是活化运移到集聚成矿的基本动力保证，构造应力场的转移是其重要体现。牡丹河岩石圈断层活动地幔发生了阳极化过程。这个过程激活并转移了矿物质，成为了它们的主要驱动力。该过程是发生岩性作用和矿化的根源之一。地幔-地幔反应使地幔中的流体变成含矿流体，为流体成矿提供了矿物来源，并通过深层断层转移到较高的平流层。当物理化学条件发生变化时，流体会因沉积而矿化。 Kiamusze断层东缘的金耳带受深部破裂控制，沉积是相关的。在相同的构造应力系统下，耳相带的矿化作用完成了。与之相关的N-N-E和N-W-W是定向断裂，而海底—超海底岩体是寻找未来的方向。

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