2002Geology of ShandongRequires access

Origin and Ore-probing Direction of Songjiagou Gold Deposit in Muping Area, Yantai City

Liu Hai-ping

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Abstract

Songjiagou gold deposit occurrs in conglomerates of Pre-cretaceous Laiyang group, which is altered conglomerate type gold deposit controlled by concerntrating belt of faults and cracks. This gold deposit is a hidden one, and has the same characteristics with Pengjiakuang altered rocks type gold deposit occurring at the edge of basin. The major control factors of the deposit are faults, and the ore-forming age is late Yanshan period of Mesozoic.

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Songjiagou gold deposit occurrs in conglomerates of Pre-cretaceous Laiyang group, which is altered conglomerate type gold deposit controlled by concerntrating belt of faults and cracks. This gold deposit is a hidden one, and has the same characteristics with Pengjiakuang altered rocks type gold deposit occurring at the edge of basin. The major control factors of the deposit are faults, and the ore-forming age is late Yanshan period of Mesozoic.

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Available abstract

Songjiagou gold deposit occurrs in conglomerates of Pre-cretaceous Laiyang group, which is altered conglomerate type gold deposit controlled by concerntrating belt of faults and cracks. This gold deposit is a hidden one, and has the same characteristics with Pengjiakuang altered rocks type gold deposit occurring at the edge of basin. The major control factors of the deposit are faults, and the ore-forming age is late Yanshan period of Mesozoic.

Key concepts: Geology, Cretaceous, Conglomerate, Geochemistry, Mesozoic, Gold ore, Structural basin, Mining engineering

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Origin and Ore-probing Direction of Songjiagou Gold Deposit in Muping Area, Yantai City — Research Paper | ScholarLens