A suite of sedimentary-volcaniclastic rocks intercalated with the volcanic rocks unconformably overlies the Triassic Xiaochaka Formation in the Woruo Mountain region, Qiangtang Basin, northern Tibet. The vitric tuff f...A suite of sedimentary-volcaniclastic rocks intercalated with the volcanic rocks unconformably overlies the Triassic Xiaochaka Formation in the Woruo Mountain region, Qiangtang Basin, northern Tibet. The vitric tuff from the base of these strata gives a SHRIMP zircon U-Pb age of 216 ± 4.5 Ma, which represents the age of the Late Triassic volcanic-sedimentary events in the Woruo Mountain region, and is consistent with that of the formation of the volcanic rocks from the Nadi Kangri Formation in the Nadigangri-Shishui River zone. There is a striking similarity in geochemical signatures of the volcanic rocks from the Woruo Mountain region and its adjacent Nadigangri-Shishui River zone, indicating that all the volcanic rocks from the Qiangtang region might have the same magmatic source and similar tectonic setting during the Late Triassic. The proper recognition of the Late Triassic large-scale volcanic eruption and volcanic-sedimentary events has important implications for the interpretation of the Late Triassic biotic extinction, climatic changes and regressive events in the eastern Tethyan domain, as well as the understanding of the initiation and nature, and sedimentary features of the Qiangtang Basin during the Late Triassic-Jurassic.展开更多
Unconsolidated siliciclastic sediments can undergo post-burial deformation, which leads to the formation of distinctive sedimentary structures, known as soft-sediment deformation structures(SSDS). The presence of a se...Unconsolidated siliciclastic sediments can undergo post-burial deformation, which leads to the formation of distinctive sedimentary structures, known as soft-sediment deformation structures(SSDS). The presence of a series of sand volcanoes confined to a particular lithostratigraphic horizon can represent a paleoseismic activity and, thereby, exemplifies the concept of “seismite”. The Kutch Basin has been a tectonically active region since the initiation of eastern Gondwana rifting followed by a tectonic inversion during the Cenozoic due to the collision of the Indian and Eurasian plates. A stratum-bound series of sand volcanoes belonging to the Khari Nadi Formation(KNF) is exposed along the banks of Khari River. They separate the shallow marine deposits below and non-marine deposits above with their characteristic marine and paleosol trace fossil suites, respectively. Although a seismogenic origin has been much debated for the SSDS,the ichnofabric analysis of the sand-volcano-bearing stratum unequivocally points toward such an origin under a shallow seafloor condition. In addition to the sedimentary regime change from an open shallow-marine setting to a continental depositional environment concomitant with basinal uplift, the behavior of the burrowing crustaceans testifies to a syn-depositional development of a fault network associated with the fluidization, sand volcanism, and the resilience of the trace-producers in surviving those processes until the sedimentary regime change in the overlying strata. Although the ichno-sedimentological evidence apparently differs from the previous works that proposed a continuous base-level rise from the beginning of deposition of the Khari Nadi Formation up to the middle part of the overlying Chhasra Formation, the paleoseismic activity,its ichnologic signature, and the depositional regime change refer to a higher-resolution(i.e., lower-order)sequence-stratigraphic change causing a short-duration regression within a longer-duration cycle of base-level rise.展开更多
鉴于UIC初运行所具有的特性及在动车通信网络中的重要作用,依据UIC556协议规范,详细地分析UIC初运行的算法和工作原理,以此为基础,首先利用CSS(Configuration Service Station)软件配置网关中对应车辆的静态属性、车辆类型,车辆支持的...鉴于UIC初运行所具有的特性及在动车通信网络中的重要作用,依据UIC556协议规范,详细地分析UIC初运行的算法和工作原理,以此为基础,首先利用CSS(Configuration Service Station)软件配置网关中对应车辆的静态属性、车辆类型,车辆支持的功能等重要信息并生成NSDB数据库,其次利用UIC Train Diagnostic Station软件将数据库下载到半实物仿真平台的网关中,查看CSS中UIC初运行情况。仿真结果表明实现了UIC初运行。展开更多
The study identifies the extent of soil loss and proposes a method for prioritization of micro-watershed in the Nun Nadi watershed.The study used the Sediment Yield Index(SYI)method,based on weighted overlays of soil,...The study identifies the extent of soil loss and proposes a method for prioritization of micro-watershed in the Nun Nadi watershed.The study used the Sediment Yield Index(SYI)method,based on weighted overlays of soil,topography,rainfall erosivity and land use parameters in 24 micro watersheds.Accordingly the values and thematic layers were integrated as per the SYI model,and minimum and maximum sediment yield values were calculated.The priority ranks as per the sediment yield values were assigned to all micro-watersheds.Then the values were classified into four priority zones according to their composite scores.Almost 14 percent area of three micro-watersheds(SW5b,SW6a and SW7b)showed very high priority;approximately 30.57 percent of the study area fell under the high priority zones.These areas require immediate attention.Conservation methods are suggested,and the locations of check dams are proposed after considering drainage,slope and soil loss.&2015 International Research and Training Center on Erosion and Sedimentation and China Water and Power Press.Production and Hosting by Elsevier B.V.This is an open access article under the CC BY-NC-ND license(http://creativecommons.org/licenses/by-nc-nd/4.0/).展开更多
基金the National Oil and Gas Special Project(Keyou [2006] No.2)"the National Natural Science Foundation of China (Grant No. 40472070)
文摘A suite of sedimentary-volcaniclastic rocks intercalated with the volcanic rocks unconformably overlies the Triassic Xiaochaka Formation in the Woruo Mountain region, Qiangtang Basin, northern Tibet. The vitric tuff from the base of these strata gives a SHRIMP zircon U-Pb age of 216 ± 4.5 Ma, which represents the age of the Late Triassic volcanic-sedimentary events in the Woruo Mountain region, and is consistent with that of the formation of the volcanic rocks from the Nadi Kangri Formation in the Nadigangri-Shishui River zone. There is a striking similarity in geochemical signatures of the volcanic rocks from the Woruo Mountain region and its adjacent Nadigangri-Shishui River zone, indicating that all the volcanic rocks from the Qiangtang region might have the same magmatic source and similar tectonic setting during the Late Triassic. The proper recognition of the Late Triassic large-scale volcanic eruption and volcanic-sedimentary events has important implications for the interpretation of the Late Triassic biotic extinction, climatic changes and regressive events in the eastern Tethyan domain, as well as the understanding of the initiation and nature, and sedimentary features of the Qiangtang Basin during the Late Triassic-Jurassic.
基金Science and Engineering Research Board (SERB), Government of India (Grant # CRG/2018/000259 to SDG)Industrial Research and Consultancy Centre (IRCC), IIT Bombay (Seed Grant # RD/0517-IRCCSH0-035 to SDG)Council of Scientific and Industrial Research (CSIR) (doctoral scholarship for AS),University Grants Commission (doctoral scholarship for KC),IIT Bombay and Ministry of Education of India (doctoral scholarship for MD)。
文摘Unconsolidated siliciclastic sediments can undergo post-burial deformation, which leads to the formation of distinctive sedimentary structures, known as soft-sediment deformation structures(SSDS). The presence of a series of sand volcanoes confined to a particular lithostratigraphic horizon can represent a paleoseismic activity and, thereby, exemplifies the concept of “seismite”. The Kutch Basin has been a tectonically active region since the initiation of eastern Gondwana rifting followed by a tectonic inversion during the Cenozoic due to the collision of the Indian and Eurasian plates. A stratum-bound series of sand volcanoes belonging to the Khari Nadi Formation(KNF) is exposed along the banks of Khari River. They separate the shallow marine deposits below and non-marine deposits above with their characteristic marine and paleosol trace fossil suites, respectively. Although a seismogenic origin has been much debated for the SSDS,the ichnofabric analysis of the sand-volcano-bearing stratum unequivocally points toward such an origin under a shallow seafloor condition. In addition to the sedimentary regime change from an open shallow-marine setting to a continental depositional environment concomitant with basinal uplift, the behavior of the burrowing crustaceans testifies to a syn-depositional development of a fault network associated with the fluidization, sand volcanism, and the resilience of the trace-producers in surviving those processes until the sedimentary regime change in the overlying strata. Although the ichno-sedimentological evidence apparently differs from the previous works that proposed a continuous base-level rise from the beginning of deposition of the Khari Nadi Formation up to the middle part of the overlying Chhasra Formation, the paleoseismic activity,its ichnologic signature, and the depositional regime change refer to a higher-resolution(i.e., lower-order)sequence-stratigraphic change causing a short-duration regression within a longer-duration cycle of base-level rise.
文摘The study identifies the extent of soil loss and proposes a method for prioritization of micro-watershed in the Nun Nadi watershed.The study used the Sediment Yield Index(SYI)method,based on weighted overlays of soil,topography,rainfall erosivity and land use parameters in 24 micro watersheds.Accordingly the values and thematic layers were integrated as per the SYI model,and minimum and maximum sediment yield values were calculated.The priority ranks as per the sediment yield values were assigned to all micro-watersheds.Then the values were classified into four priority zones according to their composite scores.Almost 14 percent area of three micro-watersheds(SW5b,SW6a and SW7b)showed very high priority;approximately 30.57 percent of the study area fell under the high priority zones.These areas require immediate attention.Conservation methods are suggested,and the locations of check dams are proposed after considering drainage,slope and soil loss.&2015 International Research and Training Center on Erosion and Sedimentation and China Water and Power Press.Production and Hosting by Elsevier B.V.This is an open access article under the CC BY-NC-ND license(http://creativecommons.org/licenses/by-nc-nd/4.0/).
