CAJ | 학술논문

2008年以来,滇西澜沧老厂矿区深部新发现巨厚斑岩型钼矿体,找矿取得重大突破.在对矿区矿化系统结构研究的基础上,应用锆石SHRIMP U-Pb法和辉钼矿Re-Os同位素测年法对成岩和成矿进行精确定年.结果表明:成矿花岗斑岩体的形成年龄为(44.6±1.1)Ma;辉钼矿Re-Os等时线年龄为(43.78±0.78)Ma.证实矿区喜山期存在与隐伏花岗斑岩有关的大规模成矿作用,斑岩钼矿的成岩成矿期与滇西新生代岩浆作用高峰期吻合,老厂斑岩钼矿形成于陆内碰撞造山环境.
2008년이래,전서란창로엄광구심부신발현거후반암형목광체,조광취득중대돌파.재대광구광화계통결구연구적기출상,응용고석SHRIMP U-Pb법화휘목광Re-Os동위소측년법대성암화성광진행정학정년.결과표명:성광화강반암체적형성년령위(44.6±1.1)Ma;휘목광Re-Os등시선년령위(43.78±0.78)Ma.증실광구희산기존재여은복화강반암유관적대규모성광작용,반암목광적성암성광기여전서신생대암장작용고봉기문합,로엄반암목광형성우륙내팽당조산배경.
The Laochang region in western Yunnan is one of the areas with significant breakthrough for new discovery of great thick porphyry molybdenum ore bodies in the deep since 2008. On the basis of the analysis to mineralizing system texture, the rock- and ore-forming ages of the granite-porphyry and related molybdenum ores were precisely redefined by the SHRIMP zircon U-Pb and molybdenite Re-Os dating method. The results show that the age of ore-forming granite-porphyry is (44.6±1.1)Ma, and the Re-Os isochron of molybdenites is (43.78±0.78)Ma. It is suggested that a large-scale Mo(Cu)-mineralization exists in this region, which related to Himalayan concealed granite-porphyry,and consistent with the peak period of Cenozoic magmatism-mineralization in forming ages, and formed in intracontinental collision orogenic setting.