东昆仑五龙沟金矿床成矿热历史的裂变径迹热年代学证据

袁万明; 王世成; 王兰芬

doi:10.3321/j.issn:1006-3021.2000.04.008

, ,

文章导航 > 地球学报 > 2000 > (4): 389-395

袁万明, 王世成, 王兰芬. 东昆仑五龙沟金矿床成矿热历史的裂变径迹热年代学证据[J]. 地球学报, 2000, (4): 389-395. doi: 10.3321/j.issn:1006-3021.2000.04.008

引用本文:

袁万明, 王世成, 王兰芬. 东昆仑五龙沟金矿床成矿热历史的裂变径迹热年代学证据[J]. 地球学报, 2000, (4): 389-395. doi: 10.3321/j.issn:1006-3021.2000.04.008

Yuan Wanming, Wang Shicheng, Wang Lanfen. Metallogenic Thermal History of the Wulonggou Gold Deposits in East Kunlun Mountains in the Light of Fission Track Thermochronology[J]. Acta Geoscientica Sinica, 2000, (4): 389-395. doi: 10.3321/j.issn:1006-3021.2000.04.008

Citation:

Yuan Wanming, Wang Shicheng, Wang Lanfen. Metallogenic Thermal History of the Wulonggou Gold Deposits in East Kunlun Mountains in the Light of Fission Track Thermochronology[J]. Acta Geoscientica Sinica, 2000, (4): 389-395. doi: 10.3321/j.issn:1006-3021.2000.04.008