CAJ | 학술논문

系统研究了鹿湖嶂矿区的地质背景以及岩浆活动造成区域变质作用对矿床成因影响,论述矿区的控矿因素及围岩蚀变,并对该矿床成因做了探讨,认为鹿湖嶂矿区锡铁的成矿作用,与中生界三叠系上统大顶群、大顶第3层钙铁质泥板岩、燕山三期黑云母花岗岩有密切的联系.并从地质角度和物探手段对矿区的找矿标志进行了阐述.
계통연구료록호장광구적지질배경이급암장활동조성구역변질작용대광상성인영향,논술광구적공광인소급위암식변,병대해광상성인주료탐토,인위록호장광구석철적성광작용,여중생계삼첩계상통대정군、대정제3층개철질니판암、연산삼기흑운모화강암유밀절적련계.병종지질각도화물탐수단대광구적조광표지진행료천술.
The geological background of the Luhuzhang deposit was extensively investigated, and the effects of the geological degeneration of the mine area due to the magma activities on the deposit formation were discussed in the paper. It was shown that the mineralization of the Luhuzhang stannum-iron deposit was closely related to the Triassic series upper Dading group of the Mesozoic Era, the calcium-iron shale in the Dading third stratum, and the biotite granite of the Yanshan third period. The prospecting indications based on geological and physical surveys were described as well.