The Gangdese batholith, more than 2500 km in length, is composed mainly of JurassicMiocene igneous rocks. This batholith is one of the most important constituents of the Tibetan orogenesis and provides an ideal place ...The Gangdese batholith, more than 2500 km in length, is composed mainly of JurassicMiocene igneous rocks. This batholith is one of the most important constituents of the Tibetan orogenesis and provides an ideal place for study of Neo-Tethyan ocean geodynamic evolution and plateau uplift. Recent studies on the Gangdese Jurassic felsic magmatism highlight its juvenile source. However, important aspects concerning the genesis of the juvenile magmatism and related deep geodynamic evolution are still unclear. Here, we report detailed petrological, geochronological, geochemical, whole-rock Sr-Nd isotopic, and in situ Sr-Hf isotopic data for a recently identified hornblende gabbro in the Dongga area, southern Lhasa sub-block. This hornblende gabbro is dominated by hornblende and plagioclase, dated at Early Jurassic(ca. 180–190 Ma), and characterized by a narrow compositional range in SiO2(49.38wt%–52.27wt%), MgO(4.08wt%–7.00wt%), FeO(10.43wt%–11.77wt%), Na2O(2.58wt%–3.51wt%), and K2O(0.48wt%–1.53wt%). It has depleted isotopic signatures, with whole-rock(87Sr/86Sr)i ratios of 0.7033–0.7043, εNd(t) values of +4.90 to +6.99, in situ plagioclase(87Sr/86Sr)i ratios of 0.7034–0.7042, and zircon εHf(t) of +12.2 to +16.8. Our results integrated with published data suggest a model of Gangdese juvenile crustal growth by a subduction-related water-enriched mantle wedge. The hydrous partial melting of the lithosphere mantle was triggered by the dehydration of a Neo-Tethyan oceanic slab. This mafic magmatism emplaced in the middle-lower crust of intraoceanic arcs or active continental margins, leading to Jurassic juvenile crustal growth in southern Tibet.展开更多
在浏览器/服务器(Browser/Server,B/S)环境下,文章主要研究三维可视化平台,设计了基于Cesium地图引擎,采用Vue和Element UI作为界面框架,后台通过GeoServer、Tomcat搭建地理信息系统(Geographic Information System,GIS)服务,利用前后...在浏览器/服务器(Browser/Server,B/S)环境下,文章主要研究三维可视化平台,设计了基于Cesium地图引擎,采用Vue和Element UI作为界面框架,后台通过GeoServer、Tomcat搭建地理信息系统(Geographic Information System,GIS)服务,利用前后端分离的技术完成组件化的三维可视化基础信息平台。整个体系设计采用开源框架,根据软件工程的设计思想,阐述三维可视化平台的总体设计思想和框架,并给出了相关的架构图。展开更多
基金jointly supported by The National Key Research and Development Project of China(2016YFC0600310)National Science Foundation of China(4132010400441672197 and 41302054)
文摘The Gangdese batholith, more than 2500 km in length, is composed mainly of JurassicMiocene igneous rocks. This batholith is one of the most important constituents of the Tibetan orogenesis and provides an ideal place for study of Neo-Tethyan ocean geodynamic evolution and plateau uplift. Recent studies on the Gangdese Jurassic felsic magmatism highlight its juvenile source. However, important aspects concerning the genesis of the juvenile magmatism and related deep geodynamic evolution are still unclear. Here, we report detailed petrological, geochronological, geochemical, whole-rock Sr-Nd isotopic, and in situ Sr-Hf isotopic data for a recently identified hornblende gabbro in the Dongga area, southern Lhasa sub-block. This hornblende gabbro is dominated by hornblende and plagioclase, dated at Early Jurassic(ca. 180–190 Ma), and characterized by a narrow compositional range in SiO2(49.38wt%–52.27wt%), MgO(4.08wt%–7.00wt%), FeO(10.43wt%–11.77wt%), Na2O(2.58wt%–3.51wt%), and K2O(0.48wt%–1.53wt%). It has depleted isotopic signatures, with whole-rock(87Sr/86Sr)i ratios of 0.7033–0.7043, εNd(t) values of +4.90 to +6.99, in situ plagioclase(87Sr/86Sr)i ratios of 0.7034–0.7042, and zircon εHf(t) of +12.2 to +16.8. Our results integrated with published data suggest a model of Gangdese juvenile crustal growth by a subduction-related water-enriched mantle wedge. The hydrous partial melting of the lithosphere mantle was triggered by the dehydration of a Neo-Tethyan oceanic slab. This mafic magmatism emplaced in the middle-lower crust of intraoceanic arcs or active continental margins, leading to Jurassic juvenile crustal growth in southern Tibet.
文摘在浏览器/服务器(Browser/Server,B/S)环境下,文章主要研究三维可视化平台,设计了基于Cesium地图引擎,采用Vue和Element UI作为界面框架,后台通过GeoServer、Tomcat搭建地理信息系统(Geographic Information System,GIS)服务,利用前后端分离的技术完成组件化的三维可视化基础信息平台。整个体系设计采用开源框架,根据软件工程的设计思想,阐述三维可视化平台的总体设计思想和框架,并给出了相关的架构图。