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NING Chuanxiang MA Zhongliang JIANG Zhenxue SU Siyuan LI Tingwei ZHENG Lunju WANG Guozhen LI Fengxun 《《地质学报》英文版》2020,94(2):352-363
To reveal the effect of shale reservoir characteristics on the movability of shale oil and its action mechanism in the lower third member of the Shahejie Formation(Es3l), samples with different features were selected and analyzed using N2 adsorption, high-pressure mercury injection capillary pressure(MICP), nuclear magnetic resonance(NMR), high-speed centrifugation, and displacement image techniques. The results show that shale pore structure characteristics control shale oil movability directly. Movable oil saturation has a positive relationship with pore volume for radius > 2 μm, as larger pores often have higher movable oil saturation, indicating that movable oil is present in relatively larger pores. The main reasons for this are as follows. The relatively smaller pores often have oil-wetting properties because of organic matter, which has an unfavorable effect on the flow of oil, while the relatively larger pores are often wetted by water, which is helpful to shale oil movability. The rich surface provided by the relatively smaller pores is beneficial to the adsorption of immovable oil. Meanwhile, the relatively larger pores create significant pore volume for movable oil. Moreover, the larger pores often have good pore connectivity. Pores and fractures are interconnected to form a complex fracture network, which provides a good permeability channel for shale oil flow. The smaller pores are mostly distributed separately;thus, they are not conducive to the flow of shale oil. The mineral composition and fabric macroscopically affect the movability of shale oil. Calcite plays an active role in shale oil movability by increasing the brittleness of shale and is more likely to form micro-cracks under the same stress background. Clay does not utilize shale oil flow because of its large specific surface area and its block effect. The bedding structure increases the large-scale storage space and improves the connectivity of pores at different scales, which is conducive to the movability of shale oil. 相似文献
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蒙古塔木察格盆地塔南凹陷下白垩统层序结构类型、控制因素与层序发育模式 总被引:5,自引:0,他引:5
利用录井及地震反射资料,采用层序地层学原理对蒙古塔木察格盆地塔南凹陷下白垩统地层层序进行了划分和对比,划分出了4个三级层序(SQ1-SQ4)。在此基础上,结合盆地的构造演化特点,研究了层序结构特征,划分了层序类型,其中,SQ1和SQ2为初始裂谷期湖泊层序,SQ3为裂谷深陷期层序,SQ4为裂谷后过渡层序。层序的结构主要受构造沉降方式控制,塔南凹陷不同时期构造沉降方式不同,形成了3种层序发育模式,即简单箕状斜坡模式、差异沉降构造反转模式、坳陷型层序发育模式,不同的层序发育模式,其地层岩性圈闭的发育和分布不同。 相似文献
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Magma underplating and Hannuoba present crust-mantle transitional zone composition: Xenolith petrological and geochemical evidence 总被引:7,自引:0,他引:7
FAN Qicheng ZHANG Hongfu SUI Jianli ZHAI Mingguo SUN Qian & LI Ni . Institute of Geology Geophysics Chinese Academy of Sciences Beijing China . Institute of Geology China Seismological Bureau Beijing China 《中国科学D辑(英文版)》2005,48(8):1089-1105
Studies on the deep-seated xenoliths from global volcanoes reveal that the present petrological crust-mantle boundary between the lower crust and the upper mantle actually is a transitional layer from mainly mafic granulites to ultramafic spinel lher-zolites[1,2], i.e. a transitional zone distinctive from the seismological Moho[3]. Oceanic lithosphere crust- mantle transitional zone can be established from the study on the exposed ophiolites. However, as for the continental lithosphere, since … 相似文献
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巴西地处南大西洋沿岸特殊的地理位置,深水海洋油气技术先进,产业区域性聚集明显,受极地气候变化影响明显,在此大背景下,巴西政府高度重视海洋与极地发展对其国际地位、政府治理、产业经济和社会稳定的联动影响。近年来,巴西借助部际海洋资源委员会、南极事务委员会等专业管理和决策机构,颁布了一系列海洋与极地战略的政策规划和法律法规,旨在全面推动巴西在全球海洋与极地科技事务中的顶层部署和研究领域,尤其是费拉兹司令南极科学考察站的建成,为巴西参与南极事务奠定了基础设施和支撑。中国可在借鉴巴西海洋与极地事务经验教训的基础上,特别是深水油气开发技术的成功经验上,持续加强与巴西的深层合作,积极寻求两国在海洋与极地科技开发中的相互战略支持,建立和谐稳定的中巴双边科技创新长效合作机制,更加有利于中国海洋与极地科技创新的全面发展。 相似文献
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YE Huping ZHANG Bing LIAO Xiaohan LI Tongji SHEN Qian ZHANG Fangfang ZHU Jianhua LI Junsheng 《中国海洋湖沼学报》2019,(5)
The absorption spectrum of phytoplankton is an important bio-optical parameter for ocean color hyperspectral remote sensing;its magnitude and shape can be affected considerably by pigment composition and concentration.We conducted Gaussian decomposition to the absorption spectra of phytoplankton pigment and studied the spectral components of the phytoplankton,in which the package effect was investigated using pigment concentration data and phytoplankton absorption spectra.The decomposition results were compared with the corresponding concentrations of the five main pigment groups(chlorophylls a,b,and c,photo-synthetic carotenoids(PSC),and photo-protective carotenoids(PPC)).The results indicate that the majority of residual errors in the Gaussian decomposition are0.001 m~(-1),and R~2 of the power regression between characteristic bands and HPLC pigment concentrations(except for chlorophyll b)was0.65 or greater for surface water samples at autumn cruise.In addition,we determined a strong predictive capability for chlorophylls a,c,PPC,and PSC.We also tested the estimation of pigment concentrations from the empirical specific absorption coefficient of pigment composition.The empirical decomposition showed that the Ficek model was the closest to the original spectra with the smallest residual errors.The pigment decomposition results and HPLC measurements of pigment concentration are in a high consistency as the scatter plots are distributed largely near the 1:1 line in spite of prominent seasonal variations.The Wozniak model showed a better fit than the Ficek model for Chla,and the median relative error was small.The pigment component information estimated from the phytoplankton absorption spectra can help better remote sensing of hyperspectral ocean color that related to the changes in phytoplankton communities and varieties. 相似文献