Supercritical CO2appearing as bubbles in hydrothermal vents was identified in the south part of the Okinawa Trough using in situ Raman spectroscopy. Significantly, the N2peak in supercritical CO2is much larger than th...Supercritical CO2appearing as bubbles in hydrothermal vents was identified in the south part of the Okinawa Trough using in situ Raman spectroscopy. Significantly, the N2peak in supercritical CO2is much larger than those in seawater and vent fluids, indicating that supercritical CO2enriches N2from the surrounding environment. Considering that the partial pressures of CO2and N2in the Earth’s protoatmosphere were 10–20 MPa, supercritical CO2with high N2was likely the dominant CO2phase near the water-air interface in the early history of the Earth, which promoted the synthesis, pre-enrichment and preservation of amino acids and other organic matters that are essential to the origin of life.展开更多
西南印度洋中脊(Southwest Indian Ridge,SWIR)热液区具有潜在发育的大规模硫化物矿床,当前正在开展SWIR硫化物矿产资源评价。测量分析硫化物和不同围岩的声速等物性特征是硫化物近底地震勘探资料处理和解释的基础。该文对西南印度洋中...西南印度洋中脊(Southwest Indian Ridge,SWIR)热液区具有潜在发育的大规模硫化物矿床,当前正在开展SWIR硫化物矿产资源评价。测量分析硫化物和不同围岩的声速等物性特征是硫化物近底地震勘探资料处理和解释的基础。该文对西南印度洋中脊热液区的硫化物和围岩等样品进行了系统的物性测量,结合岩石物性(包括密度、孔隙度、P波速度)与矿物组成,深入分析了西南印度洋中脊热液区岩石声速变化特性及其影响因素。结果表明,SWIR热液区围岩的P波速度受到岩石骨架矿物、孔隙和围压的影响。由于岩石孔隙度总体偏小,对P波速度的影响并不显著,但围压的增加使岩石微裂缝和孔隙逐渐闭合,P波速度呈非线性指数变化。蚀变作用导致了矿物成分改变,是影响围岩声速的最关键因素。单一物性参数测量结果可能存在多解性,联合波速、密度、磁性和电性等多物性参数测量有利于岩性区分。该研究成果有助于识别硫化物和围岩,为我国西南印度洋合同区多金属硫化物地震勘探工作提供重要支撑。展开更多
基金This work was supported by the Strategic Priority Research Program of Chinese Academy of Sciences(XDA22050100),the National Natural Science Foundation of China(NSFC,41822604,41576104),the National Key Research and Development Program of China(2016YFC0302103)the Key Research Program of Frontier Sciences,of Chinese Academy of Sciences(QYZDB-SSW-DQC004)+2 种基金the NSFC-Shandong Joint Fund for Marine Science Research Centers(U1606401)the Young Taishan Scholars Program(tsqn201909158)the Laboratory for Marine Geology,Pilot National Laboratory for Marine Science and Technology(Qingdao)(MGQNLM-TD201904).Any additional data can be obtained from Xin Zhang.
文摘Supercritical CO2appearing as bubbles in hydrothermal vents was identified in the south part of the Okinawa Trough using in situ Raman spectroscopy. Significantly, the N2peak in supercritical CO2is much larger than those in seawater and vent fluids, indicating that supercritical CO2enriches N2from the surrounding environment. Considering that the partial pressures of CO2and N2in the Earth’s protoatmosphere were 10–20 MPa, supercritical CO2with high N2was likely the dominant CO2phase near the water-air interface in the early history of the Earth, which promoted the synthesis, pre-enrichment and preservation of amino acids and other organic matters that are essential to the origin of life.
文摘西南印度洋中脊(Southwest Indian Ridge,SWIR)热液区具有潜在发育的大规模硫化物矿床,当前正在开展SWIR硫化物矿产资源评价。测量分析硫化物和不同围岩的声速等物性特征是硫化物近底地震勘探资料处理和解释的基础。该文对西南印度洋中脊热液区的硫化物和围岩等样品进行了系统的物性测量,结合岩石物性(包括密度、孔隙度、P波速度)与矿物组成,深入分析了西南印度洋中脊热液区岩石声速变化特性及其影响因素。结果表明,SWIR热液区围岩的P波速度受到岩石骨架矿物、孔隙和围压的影响。由于岩石孔隙度总体偏小,对P波速度的影响并不显著,但围压的增加使岩石微裂缝和孔隙逐渐闭合,P波速度呈非线性指数变化。蚀变作用导致了矿物成分改变,是影响围岩声速的最关键因素。单一物性参数测量结果可能存在多解性,联合波速、密度、磁性和电性等多物性参数测量有利于岩性区分。该研究成果有助于识别硫化物和围岩,为我国西南印度洋合同区多金属硫化物地震勘探工作提供重要支撑。
