The Emeishan continental flood basalt, which is widespread in Yunnan, Guizhou and Sichuan provinces of Southwest China, is the volcanic product of a Permian mantle plume, and native copper-chalcocite mineralization as...The Emeishan continental flood basalt, which is widespread in Yunnan, Guizhou and Sichuan provinces of Southwest China, is the volcanic product of a Permian mantle plume, and native copper-chalcocite mineralization associated with the basalt is very common in the border area of Yunnan and Guizhou provinces. The mineralization occurred in the tuff intercalation and terrestrial sedimentary rock intercalation which were formed during the main period of basalt eruption. The orebodies are controlled by the stratigraphic position and faults. Metal ore minerals in the ores are mainly native copper, chalcocite and tenorite, with small amounts of chalcopyrite, bomite, pyrite and malachite, and sometimes with large amounts of bitumen, carbon and plant debris. Several decades of ore deposits are distributed in the neighboring areas of the two provinces, while most of them are small-scale deposits or only ore occurrences. By comparing the lead isotopic composition of the ores with that of the wall-rocks, cover and basement rocks of various periods, the source of copper in this type of ore deposits was studied in this paper. The results showed that: (1) The Pb isotopic composition of the ores from ten deposits is absolutely different from that of siliceous-argillaceus rocks of the Upper Permian Xuanwei Formation, limestones of the Lower Permian Series and Carboniferous, Cambrian sandstone-shale and recta-sedimentary rock and dolomite from the upper part of the Meso-Proterozoic Kunyang Group. This indicates that ore lead was derived neither from the cover rock nor from the basement rocks; (2) Although the Neo-Proterozoic Siman dolomite and silicalite, and dolomite in the lower part of the Kunyang Group are similar in Pb isotopic composition to the ores, lead and copper contents in these rocks are very low and they have not made great contributions to copper mineralization; (3) The ores have the same Pb isotopic composition as the basalt, the latter being enriched in copper. These facts indicate that lead and copper were derive展开更多
云贵川草地是中国草地的重要组成部分,在我国生态文明建设和响应全球气候变化中具有重要的地位,分析其净初级生产力(NPP)变化格局具有重要意义。利用研究区的AVHRR、MODIS遥感影像等数据及周边地区的气象资料,结合改进的CASA模型,对云...云贵川草地是中国草地的重要组成部分,在我国生态文明建设和响应全球气候变化中具有重要的地位,分析其净初级生产力(NPP)变化格局具有重要意义。利用研究区的AVHRR、MODIS遥感影像等数据及周边地区的气象资料,结合改进的CASA模型,对云贵川地区草地1996~2015年20 a间的NPP及草地植被相关生态特征进行估算,并对其时空特征及影响因素进行分析。结果表明:(1)20 a间云贵川草地NDVI值变化规律性明显,97.18%的草地面积年平均NDVImax呈现增加趋势。(2)20 a间云贵川草地NPP总体上呈现出"西北低、西南高、东部居中"的空间格局,年均NPP值为420.85 g C·m-2。(3)时间格局上,20 a间整个云贵川区域逐年平均NPP值虽然有一定的波动性,但仍以7.2322 g C·m-2·a-1的速率在增加。20 a间夏季NPP平均值最高,为160.25 g C·m-2;春季次之,NPP平均值为109.10 g C·m-2;秋季与春季相比,NPP值稍低,为106.10 g C·m-2;冬季最低,为54.03 g C·m-2。展开更多
基金support of the Key Orientation Project (No. KZCX2-YW-111) of Chinese Academy of SciencesNational Basic Research Program of China (No. 2007CB411408)
文摘The Emeishan continental flood basalt, which is widespread in Yunnan, Guizhou and Sichuan provinces of Southwest China, is the volcanic product of a Permian mantle plume, and native copper-chalcocite mineralization associated with the basalt is very common in the border area of Yunnan and Guizhou provinces. The mineralization occurred in the tuff intercalation and terrestrial sedimentary rock intercalation which were formed during the main period of basalt eruption. The orebodies are controlled by the stratigraphic position and faults. Metal ore minerals in the ores are mainly native copper, chalcocite and tenorite, with small amounts of chalcopyrite, bomite, pyrite and malachite, and sometimes with large amounts of bitumen, carbon and plant debris. Several decades of ore deposits are distributed in the neighboring areas of the two provinces, while most of them are small-scale deposits or only ore occurrences. By comparing the lead isotopic composition of the ores with that of the wall-rocks, cover and basement rocks of various periods, the source of copper in this type of ore deposits was studied in this paper. The results showed that: (1) The Pb isotopic composition of the ores from ten deposits is absolutely different from that of siliceous-argillaceus rocks of the Upper Permian Xuanwei Formation, limestones of the Lower Permian Series and Carboniferous, Cambrian sandstone-shale and recta-sedimentary rock and dolomite from the upper part of the Meso-Proterozoic Kunyang Group. This indicates that ore lead was derived neither from the cover rock nor from the basement rocks; (2) Although the Neo-Proterozoic Siman dolomite and silicalite, and dolomite in the lower part of the Kunyang Group are similar in Pb isotopic composition to the ores, lead and copper contents in these rocks are very low and they have not made great contributions to copper mineralization; (3) The ores have the same Pb isotopic composition as the basalt, the latter being enriched in copper. These facts indicate that lead and copper were derive
文摘云贵川草地是中国草地的重要组成部分,在我国生态文明建设和响应全球气候变化中具有重要的地位,分析其净初级生产力(NPP)变化格局具有重要意义。利用研究区的AVHRR、MODIS遥感影像等数据及周边地区的气象资料,结合改进的CASA模型,对云贵川地区草地1996~2015年20 a间的NPP及草地植被相关生态特征进行估算,并对其时空特征及影响因素进行分析。结果表明:(1)20 a间云贵川草地NDVI值变化规律性明显,97.18%的草地面积年平均NDVImax呈现增加趋势。(2)20 a间云贵川草地NPP总体上呈现出"西北低、西南高、东部居中"的空间格局,年均NPP值为420.85 g C·m-2。(3)时间格局上,20 a间整个云贵川区域逐年平均NPP值虽然有一定的波动性,但仍以7.2322 g C·m-2·a-1的速率在增加。20 a间夏季NPP平均值最高,为160.25 g C·m-2;春季次之,NPP平均值为109.10 g C·m-2;秋季与春季相比,NPP值稍低,为106.10 g C·m-2;冬季最低,为54.03 g C·m-2。
