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Origin of dolomites in the Permian dolomitic reservoirs of Fengcheng Formation in Mahu Sag,Junggar Basin, NW China

Petroleum Exploration and Development 2023年第1期50卷 43-56页

作者： TANG Yong LYU Zhengxiang HE Wenjun QING Yuanhua LI Xiang song xiuzhang YANG Sen CAO Qinming QIAN Yongxin ZHAO Xinmei PetroChina Xinjiang Oilfield Company Karamay 834000China College of Energy Resources Chengdu University of TechnologyChengdu 610059China State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Chengdu University of TechnologyChengdu 610059China Petroleum Exploration and Development Institute PetroChina Xinjiang Oilfield CompanyKaramay 834000China School of History and Geography Chengdu Normal UniversityChengdu 611130China CNOOC Experimental Center CNOOC EnerTech-Drilling&Production Co.Tianjin 300450China Sinopec Southwest Oil&Gas Company Chengdu 610041China

Origin of authigenic dolomites in the dolomitic reservoir of the Permian Fengcheng Formation in the Mahu Sag of Junggar Basin is *** and genetic evolution of the authigenic dolomites in dolomitic rock reservoir of the Fengcheng Formation in the Mahu Sag were analyzed by polarized and fluorescence thin sections,scanning electron microscope(SEM),electron microprobe(EMP),C,O and Sr isotopes analysis,and other techniques.(1)Dolomites were mainly precipitated in three stages:penecontemporaneous-shallow burial stage(early stage of the Middle Permian),middle burial stage(middle stage of the Middle Permian),and middle-deep burial stage,with the former two stages in dominance.(2)Dolomitization fluid was high-salinity brine originating from alkaline *** the penecontemporaneous-shallow burial stage,Mg^(2+)was mainly supplied by alkaline-lake fluid and devitrification of volcanic *** the middle burial stage,Mg^(2+)mainly came from the transformation of clay minerals,devitrification of volcanic glass and dissolution of aluminosilicates such as feldspar.(3)Regular changes of Mg,Mn,Fe,Sr,Si and other elements during the growth of dolomite were mainly related to the alkaline-lake fluid,and to different influences of devitrification and diagenetic alteration of volcanic materials during the burial.(4)In the penecontemporaneous stage,induced by alkaline-lake microorganisms,the micritic-microcrystalline dolomites were formed by primary precipitation,replacement of aragonite and high-Mg calcite,and other processes;in the shallow burial stage,the silt-sized dolomites were formed by continuous growth of micritic-microcrystalline dolomite and replacement of calcites,tuffs and other substances;in the middle burial stage,the dolomites,mainly silt-and fine-sized,were formed by replacement of volcanic *** research results are referential for investigating the formation mechanism and distribution patterns of tight dolomitic reservoirs in the Mahu Sag and other

关键词： dolomitic rock dolomite origin tight oil reservoir Permian Fengcheng Formation Mahu Sag Junggar Basin fluid source fluid evolution isotopic composition

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渤海海域中部古近系深埋藏湖相高孔隙度白云岩储层特征及其成因

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天然气工业 2016年第12期36卷 10-17页

作者：吕正祥宋修章张健卿元华齐玉民金晓辉成都理工大学能源学院 "油气藏地质及开发工程"国家重点实验室.成都理工大学中国石油塔里木油田公司中海石油钻采工程研究院渤海实验中心中国石化石油勘探开发研究院

渤海湾盆地渤海海域中部古近系沙河街组中发育湖相高孔隙度白云岩储层,准确预测高孔白云岩储层的分布对该区的油气勘探具有重大意义。为此,选取石臼坨凸起沙河街组(E2s)碳酸盐岩储层薄片,进行岩石矿物学、偏光显微镜、荧光、扫描电镜、... 详细信息

渤海湾盆地渤海海域中部古近系沙河街组中发育湖相高孔隙度白云岩储层,准确预测高孔白云岩储层的分布对该区的油气勘探具有重大意义。为此,选取石臼坨凸起沙河街组(E2s)碳酸盐岩储层薄片,进行岩石矿物学、偏光显微镜、荧光、扫描电镜、阴极发光等综合分析,确定了高孔白云岩的岩石类型、成岩作用和储集空间特征。分析结果表明:高孔白云岩储层主要是生屑云岩,储集空间以残余粒间原生孔和生物体腔孔为主,成岩作用的主要特征为压实作用弱,发育衬垫白云石。进一步利用同位素地质温度、气液两相包裹体均一温度等确定了自生矿物的形成时期,再以显微荧光观察结合包裹体激光拉曼烃类检测技术,获得了烃类充注的期次。结论认为,沙河街组高孔白云岩储层发育具有3大主控因素:(1)高能沉积环境是高孔白云岩储层发育的基础;(2)渗流带—潜流带形成的早期衬垫白云石有效降低了机械压实对孔隙的破坏强度;(3)早期烃类充注有利于高孔白云岩储层的发育。

关键词：渤海湾盆地渤海海域中部古近纪深埋藏白云岩高孔隙度储集层成因

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渤海海域渤南低凸起下古生界岩溶古地貌及其对储层的控制

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山东石油化工学院学报 2023年第1期37卷 54-60页

作者：王松杨纪磊宋修章中海石油(中国)有限公司天津分公司天津300450 中海油能源发展股份有限公司工程技术分公司天津300450

渤海湾盆地渤海海域下古生界碳酸盐岩岩溶古地貌的分布特征认识的不充分,限制了对古岩溶储层油气分布规律的认识。选取渤南低凸起渤中28-1地区下古生界为研究对象,通过残余地层厚度法,叠加残留地层厚度、剥蚀厚度、压实校正等特征参数,... 详细信息

渤海湾盆地渤海海域下古生界碳酸盐岩岩溶古地貌的分布特征认识的不充分,限制了对古岩溶储层油气分布规律的认识。选取渤南低凸起渤中28-1地区下古生界为研究对象,通过残余地层厚度法,叠加残留地层厚度、剥蚀厚度、压实校正等特征参数,开展下古生界顶部古地貌形态的精细刻画,探讨古地貌对储层的控制。研究表明:研究区所处的二级古地貌单元为岩溶斜坡,进一步识别坡地、残丘、沟槽3种岩溶古地貌单元;岩溶斜坡单元的整体岩溶作用强,其中残丘和坡地溶蚀作用强烈,储集性能好,且以岩溶坡地储集性能最好,沟槽的岩溶强度较弱,但仍发育有较多溶蚀孔隙。

关键词：岩溶古地貌岩溶储层下古生界渤南低凸起渤海湾盆地

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Tectonic modes of mantle convection and their implications for Earth's tectonic evolution based on three-dimensional numerical simulations

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Science China Earth Sciences 2025年第1期68卷 270-296页

作者： song XIANG Jinshui HUANG Bingcheng WU School of Earth and Space Sciences University of Science and Technology of China CAS Center of Excellence in Comparative Planetary Studies

Five tectonic modes of mantle convection are obtained and analyzed with three-dimensional numerical models in a spherical shell domain. The five tectonic convective modes are non-plate mobile-lid, plate-like mobile-lid, episodic plate-like mobile-lid, episodic stagnant-lid, and stagnant-lid convective modes, respectively. The typical characteristics of these five tectonic modes and their numerical classification criteria based on plateness, mobility, and their standard deviations are presented and discussed. The results show that the yield stress of the lithosphere has profound effects on the tectonic convective *** the gradual increase of yield stress, the tectonic mode of mantle convection changes from one to another sequentially through the aforementioned five modes. Additionally, as the Rayleigh number increases, the range of yield stress for the platelike mobile-lid convective mode decreases, and the dimensionless transition stress between different tectonic modes ***, the dimensional transition stress between the non-plate mobile-lid convective mode and plate-like mobile-lid convective mode increases with the increase of Rayleigh number, but decreases between other tectonic modes. Furthermore, we find that the transition stress between different tectonic modes is inversely proportional to the internal heating rate, with the transition stress decreasing as the internal heating rate increases. The fitting analysis of the transition stress between tectonic modes shows that Earth's current plate tectonics correspond to a lithospheric yield stress of 150–250 MPa, which aligns with the strength of serpentinized mantle rock determined by experimental petrography. If the Archean mantle was 300°C warmer than it is today, then the Earth was in an episodic stagnant-lid convective mode. The tectonic evolution of the Earth's surface is closely related to the lithospheric strength and the process of thermal evolution. If the lithospheric strength w

关键词： Tectonic mode of mantle convection Plate-like mobile-lid convection Episodic plate-like mobile-lid convection Episodic stagnant-lid convection Plate tectonics and tectonic evolution of the Earth

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Molecular dynamics simulations of helium transport through inorganic mineral nanopores

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Science China Earth Sciences 2025年第1期68卷 237-252页

作者： Dandan song Ping GUAN Chi ZHANG Jiahao REN School of Earth and Space Sciences Peking University

Helium transport through nanoscale inorganic mineral pores and pore throats is essential for its overall migration. To elucidate helium's transport dynamics within nanopores, we employed equilibrium and non-equilibrium molecular dynamics simulations to investigate helium's static self-diffusion and pressure-driven flow in quartz slit-shaped nanopores. We also introduced water and various gases, including hydrogen, methane, ethane, nitrogen, and carbon dioxide, into the nanopores to assess their influence on helium transport. Our findings indicate minimal helium adsorption on quartz pore surfaces. Under conditions where the pore size is less than 5 nm and the pressure under 10 MPa, environmental factors markedly influence helium diffusion. Large pore sizes, high temperatures, and low gas pressures enhance helium desorption and facilitate faster diffusion. We observed a positive correlation between helium flow velocity and factors such as pore size, pressure gradient, and surface smoothness of the pores. Notably, the presence of pore water and carrier gases in quartz nanopores, which diffuse more slowly than helium, tends to reduce helium surface adsorption and slow its diffusion. Among the carrier gases studied, nitrogen showed similar adsorption capacity, diffusivity, and stability to helium, while carbon dioxide displayed the highest adsorption capacity and the slowest diffusion rate, markedly differing from helium. Based on the simulation results, we concluded that water and carrier gases primarily function as transport mediums in helium migration, moving together with helium. Nitrogen, which shares similar properties with helium, effectively assists in this co-migration process. Conversely, carbon dioxide, due to its high adsorption capacity and slow diffusion, tends to be lost during co-migration. As a result, gas reservoirs with high nitrogen levels and low carbon dioxide levels are more likely to have higher helium concentrations. Additionally, the smaller por

关键词： Helium transport Slit nanopores Molecular dynamics simulations Diffusion Flow carriers

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CAF-derived exosome-miR-3124-5p promotes malignant biological processes in NSCLC via the TOLLIP/TLR4-MyD88-NF-κB pathway

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Oncology Research 2025年第1期33卷 133-148页

作者： TAO SUN QINGHUA song HUA LIU Department of Respiratory and Critical Care Medicine Affiliated Hospital of Nantong UniversityMedical School of Nantong UniversityNantong226001China Department of Emergency The People’s Hospital of RugaoNantong226500China Department of Haematology The People’s Hospital of RugaoNantong226500China

Background:Lung cancer is a life-threatening disease that occurs worldwide,but is especially common in *** crucial role of the tumour microenvironment(TME)in non-small cell lung cancer(NSCLC)has attracted recent ***-associated fibroblasts(CAFs)are the main factors that contribute to the TME function,and CAF exosomes are closely linked to ***:The expression levels of miR-3124-5p and Toll-interacting protein(TOLLIP)were analysed by bioinformatics prediction combined with RT-qPCR/Western Blot *** were isolated and identified from clinical NSCLC *** electron microscopy and Western Blot were used to identify exosomes from these *** in proliferation(CCK-8 and clone formation),migration(wound healing),and invasion(transwell)of NSCLC cells were *** Luciferase reporter test was applied to clarify the binding of miR-3124-5p to *** TOLLIP/TLR4/MyD88/NF-κB pathway proteins were determined using Western blot ***:MiR-3124-5p is overexpressed in clinical tissues and cells of ***-3124-5p was dramatically enriched in CAF-derived *** experiments revealed that CAFs delivered miR-3124-5p into NSCLC cells via exosomes,stimulating cancer cell ***-3124-5p acted as a sponge to negatively regulate TOLLIP expression,which activated the TLR4/MyD88/NF-κB axis to promote the occurrence and development of *** salvage tests were performed to determine whether CAF-exosome-derived miR-3124-5p plays a pro-cancer role in NSCLC by affecting the TOLLIP signalling ***:These results provide an interesting direction for the diagnosis and therapy of NSCLC.

关键词： Non-small cell lung cancer(NSCLC) Cancer-associated fibroblasts(CAFs) Exosomes miR-3124-5p Toll-interacting protein(TOLLIP)

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渤海中部沙河街组深埋藏砂岩中优质储层成因

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地球科学前沿（汉斯） 2018年第2期8卷 215-225页

作者：尹超吕正祥宋修章成都理工大学能源学院四川成都 “油气藏地质及开发工程”国家重点实验室成都理工大学四川成都

渤海古近系湖相沙河街组砂岩储层埋深较深,主要为超过3000米以下的中深层,表现为扇三角洲沉积体系。主要岩石类型为岩屑长石砂岩和长石岩屑砂岩,长石含量较高约占40.39%,石英含量较低,仅占20.39%。成岩作用过程中,压实作用总体体现为较... 详细信息

渤海古近系湖相沙河街组砂岩储层埋深较深,主要为超过3000米以下的中深层,表现为扇三角洲沉积体系。主要岩石类型为岩屑长石砂岩和长石岩屑砂岩,长石含量较高约占40.39%,石英含量较低,仅占20.39%。成岩作用过程中,压实作用总体体现为较弱,而溶蚀作用占据主要位置。由于长石溶蚀的同时,自生矿物的形成尤其是粘土矿物和自生石英,再加上碳酸盐矿物的充填,导致孔隙度不断地减少。但总体来说,研究区砂岩物性较好,平均孔隙度20.8%,渗透率460.2 mD,能形成好的储层。另一方面,通过扫描电镜、电子显微镜、荧光分析等的观察,了解不同储层孔隙度和渗透率的特征,其目的是了解形成优质储层的原因。

关键词：湖相沙河街组砂岩储层优质储层成因

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准噶尔盆地玛湖凹陷二叠系风城组白云质岩储集层白云石成因

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石油勘探与开发 2023年第1期50卷 38-50页

作者：唐勇吕正祥何文军卿元华李响宋修章杨森曹勤明钱永新赵辛楣中国石油新疆油田公司新疆克拉玛依834000 成都理工大学能源学院成都610059 “油气藏地质及开发工程”国家重点实验室成都理工大学成都610059 中国石油新疆油田公司勘探开发研究院新疆克拉玛依834000 成都师范学院史地与旅游学院成都611130 中海油能源发展股份有限公司工程技术公司中海油实验中心天津300450 中国石油化工股份有限公司西南油气公司成都610041

针对准噶尔盆地玛湖凹陷二叠系风城组白云质岩储集层中自生白云石成因认识不清的问题,利用偏光、荧光薄片鉴定,扫描电镜分析,电子探针分析,碳、氧、锶同位素组成分析等技术,对玛湖凹陷风城组白云质岩中白云石赋存特征及成因演化进行深... 详细信息

针对准噶尔盆地玛湖凹陷二叠系风城组白云质岩储集层中自生白云石成因认识不清的问题,利用偏光、荧光薄片鉴定,扫描电镜分析,电子探针分析,碳、氧、锶同位素组成分析等技术,对玛湖凹陷风城组白云质岩中白云石赋存特征及成因演化进行深入研究。研究表明:(1)白云石发育准同生—浅埋藏期、中埋藏期和中—深埋藏期3期,主要形成于中二叠世早期的准同生—浅埋藏环境,其次是中二叠世中期的中埋藏环境。(2)白云石化流体为碱湖沉积背景下的高盐度咸水,准同生—浅埋藏期Mg2+主要由碱湖流体、火山玻璃脱玻化供给,中埋藏期Mg2+主要来自于黏土矿物转化、火山玻璃脱玻化以及长石等铝硅酸盐的溶蚀。(3)白云石生长过程中由早到晚Mg、Mn、Fe、Sr、Si等元素有规律的变化,主要与碱湖流体以及埋藏过程中风城组火山物质脱玻化、成岩蚀变的影响程度不同有关。(4)在碱湖微生物诱导作用下,准同生期泥晶—微晶白云石通过原生沉淀以及交代文石、高镁方解石等形成;浅埋藏期粉晶白云石主要由泥晶—微晶白云石的持续生长以及方解石、凝灰质等交代形成;中埋藏期白云石以粉晶、细晶为主,主要由白云石化流体对火山物质的交代形成。研究结果对玛湖凹陷及其他类似含油气区域白云石质致密储集层形成机理、发育规律的研究有一定借鉴意义。

关键词：白云岩白云石成因致密油储集层二叠系风城组玛湖凹陷准噶尔盆地流体来源流体演化同位素组成

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玛湖凹陷二叠系风城组碱湖云质岩储层成岩作用

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岩性油气藏 2022年第5期34卷 26-37页

作者：吕正祥廖哲渊李岳峰宋修章李响何文军黄立良卿元华成都理工大学能源学院成都610059 中国石油新疆油田分公司勘探开发研究院新疆克拉玛依834000 成都师范学院史地与旅游学院成都610021

通过偏光显微镜和扫描电镜观察,结合能谱、包裹体温度、同位素、X射线衍射及有机地球化学等分析方法,研究了准噶尔盆地玛湖凹陷二叠系风城组碱湖云质岩储层的成岩作用类型和成岩演化序列。研究结果表明:①玛湖凹陷二叠系风城组云质岩储... 详细信息

通过偏光显微镜和扫描电镜观察,结合能谱、包裹体温度、同位素、X射线衍射及有机地球化学等分析方法,研究了准噶尔盆地玛湖凹陷二叠系风城组碱湖云质岩储层的成岩作用类型和成岩演化序列。研究结果表明:①玛湖凹陷二叠系风城组云质岩储层为典型的碱湖沉积,发育多种云质岩类,以云质凝灰岩和云质沉凝灰岩为主。②云质岩中成岩作用类型较多,其中脱玻化作用较为普遍,析出矿物主要有硅质矿物、钙镁碳酸盐矿物、铝硅酸盐矿物和非钙镁碳酸盐类矿物等;云质岩中的溶蚀作用主要为铝硅酸盐矿物和盐类矿物的溶蚀,发育成岩缝和多期构造缝,具有3期油气充注。③研究区风城组多数云质岩演化已进入中成岩A期,少量进入中成岩B期,脱玻化作用发生在早成岩A期;发育3期白云石,主要发育于早成岩B期;非钙镁碳酸盐矿物主要形成于同生期;存在3期溶蚀作用,以中成岩A期为主;油气最早充注于早成岩B期,以中成岩B期充注时间最长。脱玻化作用、长石和非钙镁碳酸盐矿物溶蚀作用及构造形成的裂缝是玛湖凹陷风城组云质岩成储的关键。④脱玻化作用形成的孔隙为早期油气充注提供了储集空间,碱湖优质烃源岩热演化释放的酸性流体对云质岩中铝硅酸盐矿物和盐类矿物进行溶蚀,有效改善了储层的储集性能。

关键词：碱湖沉积成岩作用云质岩储层风城组二叠系玛湖凹陷准噶尔盆地

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Constraints on holographic QCD phase transitions from PTA observations

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Science China(Physics,Mechanics & Astronomy) 2025年第1期Mechanics & Astronomy) .卷 71-78页

作者： song He Li Li Sai Wang Shao-Jiang Wang Center for Theoretical Physics and College of Physics Jilin University School of Physical Science and Technology Ningbo University Max Planck Institute for Gravitational Physics (Albert Einstein Institute) CAS Key Laboratory of Theoretical Physics Institute of Theoretical Physics Chinese Academy of Sciences School of Fundamental Physics and Mathematical Sciences Hangzhou Institute for Advanced StudyUniversity of Chinese Academy of Sciences (UCAS) School of Physical Sciences University of Chinese Academy of Sciences (UCAS) Theoretical Physics Division Institute of High Energy Physics Chinese Academy of Sciences

The underlying physics of QCD phase transition in the early Universe remains largely unknown due to its strong-coupling nature during the quark-gluon plasma/hadron gas transition, yet a holographic model has been proposed to quantitatively fit the lattice QCD data while with its duration of the first-order phase transition(FoPT) left undetermined. At specific baryon chemical potential, the first-order QCD phase transition agrees with the observational constraint of baryon asymmetry. It, therefore, provides a scenario for phase transition gravitational waves(GWs) within the standard model of particle physics. If these background GWs could contribute dominantly to the recently claimed common-spectrum red noise from pulsar timing array(PTA) observations, the duration of this FoPT can be well constrained, and the associated primordial black holes are still allowed by current observations.

关键词： pulsar timing array QCD phase transition gravitational waves primordial black holes

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