參 考 文 獻

沈保豐.1987.太古宙綠巖帶中金礦床的地質特征和找礦標志.國外前寒武紀地質，2：1-35.

沈保豐，駱輝，李雙保，李俊建，彭暁亮等.1994.華北陸臺太古宙綠巖帶地質及成礦.北京：地質出版社,74-117.

沈保豐，李俊建，毛德寶.1997.華北地臺綠巖帶地質特征類型和演化.前寒武紀研究進展，20（1）：2-11.

伍家善，耿元生，沈其韓，萬渝生，劉敦一，宋彪.1998.中朝古大陸太古宙地質特征及構造演化.北京：地質出版社，105-109.

沈保豐，毛德寶，李俊建.1997.中國綠巖帶型金礦床類型和地質特征.前寒武紀研究進展,20（4）：1-12.

駱輝，趙運起.1997.遼寧阜新排山樓金礦地質和成礦作用.前寒武紀研究進展，20（4）：13-24.

胡小蝶，陳志宏，趙彥明，王魁元.1997.河北小營盤金礦成礦時代-單顆粒鋯石U-Pb同位素年齡證據.前寒武紀研究進展,20（2）：22-28.

裴榮富等.2001.難識別及隱伏大礦、富礦資源潛力的地質評價.北京：地質出版社，72-74.

沈保豐，李俊建，翟安民，曹秀蘭.2001.與花崗巖有關的綠巖帶再生型金礦床特征.前寒武紀研究進展，24（3）：129-144.

羅鎮寬，苗來成，關康，等.2001.河北張家口水泉溝巖體SHRIMP年代學研究及其意義.地球化學，30（2）：116-122.

陸松年，李懷坤，李惠民，楊春亮，胡正德，蔣明媚.1997.金礦密集區的基底特征與成礦作用研究-以小秦嶺、冀北和膠北金礦密集區為例.北京：地質出版社，39-44.

Metallogenetic Characteristics of the Gold Deposits in the Katagreenstone Belts of China

SHEN Baofeng  LI Junjian  MAO Debao  ZHAI Anmin  CHAO Xiulan

（Tianjin Institute of Geology and Mineral Resoures, Tianjin 300170）

Abstract

The gold deposits in the katagreenstone belts of China are widely distributed in the North China Platform,especially in the middle-west margin of the North China Platform. In terms of the sources of the ore-forming material and metallogenic tectonic setting, with the consideration from combination of metallogeny and crustal evolution, those deposits, related to katagreenstone belts, may be divided into the later-sytectonic primary gold deposits and post-tectonic regenerated hydrothermal gold deposits, the latter are more distributed and possessed more prospecting potential. The greenstone, structures and granitoid rocks are control factores to the gold metallogenises of the katagreenstone belts. The mineralization often are multiple periods from Neoarchean-Paleoproterozoic to Hercynian,Yanshanian. In consequence of the development of the multiple mineralized  tectonic-magmaticactivities in East China, so that the two types of gold deposits can distributed in the different tectonic part of the gold metallogenic focus-area.

Key words: China; katagreenstone belst; gold deposits; late-syntectonic primary gold deposits; post-tectonic regenerated hyderthermal gold deposits

上一頁  [1] [2] [3] [4]