中文摘要:中国位于古亚洲、滨西太平洋和特提斯三大成矿域的交汇处，内生金矿成矿条件有利，具备了形成金矿的各种条件。巨型深断裂体系、地层、区域构造、岩浆岩体等地质因素对金矿具有明显的控制作用，金化探异常、重力场、莫霍面深度等地球化学和地球物理信息对金矿具有明显的指示作用，中生代成矿期，是我国内生金矿极为重要的成矿期。
Abstract:Lying at the convergence of three (Paleo-Asia, Circum-West Pacific and Tethyan) great metallogenic domains, China has various favorable metallogenic conditions for endogenetic gold deposits. Giant deep fault systems, strata, regional tectonic conditions, magmatic bodies and some other geological factors all play obvious ore-controlling roles in gold mineralization. Geochemical and geophysical data such as gold geochemical anomalies, gravity anomalies and Moho depths all serve as clear indicators to gold deposits. Mesozoic metallogenic epoch is an important ore-forming epoch for endogenetic gold deposits in China.
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张晓华，肖克炎，朱裕生.2004.中国内生金矿成矿规律及控矿因素[J].矿床地质,23(Z):166~169.2004.Metallogenic Regularity and Ore-controlling Factors of Endogenetic Gold Deposits in China[J].Mineral Deposits23(Z):166~169
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