坐落泰国旅游胜地芭提雅的希尔顿酒店,其中有多个常规空间的室内设计都是由Department of ARCHITECTURE负责的。这间多功能的度假酒店就坐落在芭提雅的市中心,从这里可以眺望到芭提雅的海岸。酒店包含了分别位于一层和17层的大堂，以厦D...坐落泰国旅游胜地芭提雅的希尔顿酒店,其中有多个常规空间的室内设计都是由Department of ARCHITECTURE负责的。这间多功能的度假酒店就坐落在芭提雅的市中心,从这里可以眺望到芭提雅的海岸。酒店包含了分别位于一层和17层的大堂，以厦DRIFT酒吧、EDGE餐厅和FLARE美食中心等空间。展开更多
By comparing PGE patterns of sulfide ores with that of basic-ultrabasic dikes occurring in the Dajing Cu-polymetallic deposit, we discover that there are similar positive slopes between the basic-ultrabasic dikes and ...By comparing PGE patterns of sulfide ores with that of basic-ultrabasic dikes occurring in the Dajing Cu-polymetallic deposit, we discover that there are similar positive slopes between the basic-ultrabasic dikes and the black ores composed mainly of sphalerite and galena, reflecting affinity of their source. The PGE patterns of the yellow ores composed basically of chalcopyrite, arsenopyrite and pyrite are actually different. One is close to the pattern of the mantle 1herzolite, and others resemble the pattern of the basic rocks. However, the concentrations of Ru are higher in the yellow ores, reflecting that sulfur attains or approaches saturation in their parent magma. The PGE characteristics of ores and dikes show that the magmas derived from the deep of crust and the metallogenic elements were supplied mainly by growth material of the crust. In addition, the mantle-derived magma also offered some elements.展开更多
文摘坐落泰国旅游胜地芭提雅的希尔顿酒店,其中有多个常规空间的室内设计都是由Department of ARCHITECTURE负责的。这间多功能的度假酒店就坐落在芭提雅的市中心,从这里可以眺望到芭提雅的海岸。酒店包含了分别位于一层和17层的大堂，以厦DRIFT酒吧、EDGE餐厅和FLARE美食中心等空间。
基金This work was supported by the Chinese Academy of Sciences (Grant Nos. KZCX2-104 and KZ951-A1-401)the Ministry of Science and Technology of China (pre-selected 39 project).
文摘By comparing PGE patterns of sulfide ores with that of basic-ultrabasic dikes occurring in the Dajing Cu-polymetallic deposit, we discover that there are similar positive slopes between the basic-ultrabasic dikes and the black ores composed mainly of sphalerite and galena, reflecting affinity of their source. The PGE patterns of the yellow ores composed basically of chalcopyrite, arsenopyrite and pyrite are actually different. One is close to the pattern of the mantle 1herzolite, and others resemble the pattern of the basic rocks. However, the concentrations of Ru are higher in the yellow ores, reflecting that sulfur attains or approaches saturation in their parent magma. The PGE characteristics of ores and dikes show that the magmas derived from the deep of crust and the metallogenic elements were supplied mainly by growth material of the crust. In addition, the mantle-derived magma also offered some elements.
