| Phase Equilibria Constraints on Relations of Ore-bearing Intrusions with Flood Basalts in the Panxi Region, Southwestern China |
| |
| 作者姓名： | ZHANG Zhaochong HAO Yanli AI Yu LI Ying ZHAO Li |
| |
| 作者单位： | State Key Laboratory of Geological Processes and Mineral Resources, University of Geosciences, Beijing 100083, China;Institute of Geology, Chinese Academy of Geosciences, Beijing 100037, China;State Key Laboratory of Geological Processes and Mineral Resources, University of Geosciences, Beijing 100083, China;State Key Laboratory of Geological Processes and Mineral Resources, University of Geosciences, Beijing 100083, China;State Key Laboratory of Geological Processes and Mineral Resources, University of Geosciences, Beijing 100083, China |
| |
| 基金项目： | The present study was supported by the National Basic Research Program of China (2009CB421002), National Natural Science Foundation of China (Grant No. 40473008, 40273020, 40572036), Program for New Century Excellent Talents in University (Grant No. NCET-04-0728), Project (B07011) and PCSIRT. |
| |
| 摘 要： | There are two types of temporally and spatially associated intrusions within the Emeishan large igneous province (LIP); namely, small ultramafic subvolcanic sills that host magmatic Cu-Ni-Platinum Group Element (PGE)-bearing sulfide deposits and large mafic layered intrusions that host giant Ti-V magnetite deposits in the Panxi region. However, except for their coeval ages, the genetic relations between the ore-bearing intrusions and extrusive rocks are poorly understood. Phase equilibria analysis (Q-Pl-Ol-Opx-Cpx system) has been carried out to elucidate whether ore-bearing Panzhihua, Xinjie and Limahe intrusions are co-magmatic with the picrites and flood basalts (including high-Ti, low-Ti and alkali basalts), respectively. In this system, the parental magma can be classified as silica-undersaturated olivine basalt and silica-saturated tholeiite. The equivalents of the parental magma of the Xinjie and Limahe peridotites and picrites and low-Ti basalts are silica-undersaturated, whereas the Limahe gabbro-diorites and high-Ti basalts are silica-saturated. In contrast, the Panzhihua intrusion appears to be alkali character. Phase equilibria relations clearly show that the magmas that formed the Panzhihua intrusion and high-Ti basalts cannot be co-magmatic as there is no way to derive one liquid from another by fractional crystallization. On the other hand, the Panzhihua intrusion appears to be related to Permian alkali intrusions in the region, but does not appear to be related to the alkali basalts recognized in the Longzhoushan lava stratigraphy. Comparably, the Limahe intrusion appears to be a genetic relation to the picrites, whereas the Xinjie intrusion may be genetically related to be low-Ti basalts. Additionally, the gabbro-diorites and peridotites of the Limahe intrusion are not co-magmatic, and the former appears to be derived liquid from high-Ti basalts.
|
| 关 键 词： | layered intrusions phase equalibria Cu-Ni sulfide deposit V-Ti-Fe oxide deposit Emeishan |
Phase Equilibria Constraints on Relations of Ore‐bearing Intrusions with Flood Basalts in the Panxi Region,Southwestern China |
| |
| Authors: | Zhaochong ZHANG Yanli HAO Yu AI Ying LI Li ZHAO |
| |
| Institution: | 1. State Key Laboratory of Geological Processes and Mineral Resources, University of Geosciences, Beijing 100083, China;2. Institute of Geology, Chinese Academy of Geosciences, Beijing 100037, China |
| |
| Abstract: | There are two types of temporally and spatially associated intrusions within the Emeishan large igneous province (LIP); namely, small ultramafic subvolcanic sills that host magmatic Cu‐Ni‐Platinum Group Element (PGE)‐bearing sulfide deposits and large mafic layered intrusions that host giant Ti‐V magnetite deposits in the Panxi region. However, except for their coeval ages, the genetic relations between the ore‐bearing intrusions and extrusive rocks are poorly understood. Phase equilibria analysis (Q‐Pl‐Ol‐Opx‐Cpx system) has been carried out to elucidate whether ore‐bearing Panzhihua, Xinjie and Limahe intrusions are co‐magmatic with the picrites and flood basalts (including high‐Ti, low‐Ti and alkali basalts), respectively. In this system, the parental magma can be classified as silica‐undersaturated olivine basalt and silica‐saturated tholeiite. The equivalents of the parental magma of the Xinjie and Limahe peridotites and picrites and low‐Ti basalts are silica‐undersaturated, whereas the Limahe gabbro‐diorites and high‐Ti basalts are silica‐saturated. In contrast, the Panzhihua intrusion appears to be alkali character. Phase equilibria relations clearly show that the magmas that formed the Panzhihua intrusion and high‐Ti basalts cannot be co‐magmatic as there is no way to derive one liquid from another by fractional crystallization. On the other hand, the Panzhihua intrusion appears to be related to Permian alkali intrusions in the region, but does not appear to be related to the alkali basalts recognized in the Longzhoushan lava stratigraphy. Comparably, the Limahe intrusion appears to be a genetic relation to the picrites, whereas the Xinjie intrusion may be genetically related to be low‐Ti basalts. Additionally, the gabbro‐diorites and peridotites of the Limahe intrusion are not co‐magmatic, and the former appears to be derived liquid from high‐Ti basalts. |
| |
| Keywords: | layered intrusions phase equalibria Cu‐Ni sulfide deposit V‐Ti‐Fe oxide deposit Emeishan |
|
| 点击此处可从《Acta Geologica Sinica》浏览原始摘要信息 |
| 点击此处可从《Acta Geologica Sinica》下载免费的PDF全文 |
|
