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A Discussion on the Origin of Shale Reservoir Inter-Laminar Fractures in the Shahejie Formation of Paleogene, Dongying Depression

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Journal of Earth Science 2017年第6期28卷 1064-1077页

作者： Huimin Liu Shun Zhang Guoqi Song Shoupeng Zhang Xuefeng Hao Zhonghuai Xie Ningning Xu Peng Liu Working Stations for Postdoctors of shengli oilfield SINOPEC research institute of Petroleum exploration and development Shengli Oilfield SINOPEC

This paper was conducted on the shale reservoir in the Dongying depression in the Shahejie Formation of Paleogene. Based on detailed core description, rock thin sections, argon ion polishing, scanning electron microscopy（SEM） analysis, CT scanning and carbon-oxygen isotopic test, the formation mechanism of the inter-laminar fractures（or seams） and their development conditions were discussed by comprehensive analysis of the diagenetic evolution features and the reservoir space evolution characteristics. The results show that the laminated composite pattern in Dongying depression was dominated by vertical distribution of laminated calcite and clay minerals. Contrasted to the traditional understanding, development degree of inter-laminar fractures was much lower. Pure fluid between layers cannot exist without framework minerals, and the pre-existing well connected pore or horizontal overpressure micro seam was favorable paths of fluid migration. From the points of inter-laminar fractures origin mechanism and its evolution, the so called seams, were much more complex than traditional understanding that hydrocarbon generation raised the pore pressure and led to the parallel microfractures. But the inter-laminar fractures had little relationship with that whether the lamination was developed or bedding boundary was clear or not. In fact, the shale reservoir inter-laminar fractures were not rigorous fracture. They were controlled by pre-existing inter-granular pore（or seam） or dissolved pore, which distributed along carbonate laminae boundary and were connected by later super pressure, dissolution and the seepage force. And the development conditions were burial depth（bigger than 3 000 m） and the Ro value（〉0.6%）. Discussion on its origin and evolution has important petroleum geological significance on optimizing reservoir segment and favorable target areas selection.

关键词： shale reservoir lamination inter-laminar fractures diagenesis Dongying depression Paleogene

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Structure kinematics of a transtensional basin:An example from the Linnan Subsag, Bohai Bay basin,Eastern China

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Geoscience Frontiers 2018年第3期9卷 917-929页

作者： Dong-Xiao Feng Fu Ye School of Earth Sciences and Resources China University of Geosciences (Beijing) exploration and development research institute of shengli oilfield company SINOPEC Geophysics research institute of shengli oilfield company SINOPEC

The Linnan subsag is a petroliferous, secondary tectonic unit of the Huimin sag that is located in the western part of the Jiyang depression in the Bohai Bay basin, eastern China. In this study, the authors calculated basin extensional rate and slipping displacement of boundary faults in the dip and strike directions, using seismic and drilling data. The evolution of the Linnan transtensional basin from the Eogene through the Quaternary is quantitatively described, and a dynamic model is established. The Linshan and Xiakou boundary faults of the Linnan subsag are used as a case study to describe a method to calculate the strike and dip slipping displacements of active faults under oblique extension. The results quantitatively illustrate the behavior of the Linnan subsag boundary faults over time. The Linnan subsag transtensional basin experienced four stages of evolution: weak extension during the Kongdian Formation, rapid extension and fault depression during the fourth member of the Shahejie Formation,intensive transtension and fault depression during the third member of the Shahejie Formation-Dongying Formation, and weakening fault depression during the Guantao Formation-Pingyuan *** results of this study provide further understanding of the processes of petroleum migration and accumulation in the region.

关键词： Transtensional basin Fault activity Quantitative calculation Basin evolution model Linnan subsag Bohai Bay basin

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Formation mechanism of carbonates in the lacustrine muddy shale and it implication for shale oil and gas: A case study of source rocks in Member 4 and Member 3 of Shahejie Formation, Dongying sag

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Petroleum research 2018年第3期3卷 248-258页

作者： Yong Wang Huiming Liu Guoqi Song Xuefeng Hao Deshun Zhu Deyan Zhu exploration and development institute Sinopec Shengli Oilfield CompanyShandong 257015China Sinopec shengli oilfield company Shandong 257001China

Through analysis of microscopic characteristics,mineral components,elements and isotopes,the genetic mechanism of carbonates in the deep lacustrine source rocks in the upper submember of Member 4 and lower submember of Member 3 of Shahejie Formation in Dongying sag,is well *** results show that four types of carbonates in the deep lake,i.e.,lenticular coarse crystalline carbonate,lamellar micro-fine crystalline carbonate,lamellar cryptocrystalline carbonate and massive cryptocrystalline *** which,the lenticular coarse crystalline carbonate is formed by diagenetic *** the lamellar micro-fine crystalline carbonate and the lamellar cryptocrystalline carbonate,through the alga photosynthesis,the carbon dioxide(CO_(2))is constantly extracted from water,thus the concentration of CO_(3)^(-2) ion in water increases,and then the CO_(3)^(-2) ion reacts with Ca2+ ion in lake water surface to form the carbonates;the saline water environment is favorable for preservation of carbonate particles which mostly occur in lamellar micro-fine crystalline;in the brackish water environment,the water is deep,and the carbonate crystalline beneath the carbonate compensation depth surface is usually is dissolved,and most of lamellar cryptocrystalline are *** massive cryptocrystalline carbonate is formed by the sedimentary carbonate which transport from shallow water to deep water by gravity *** some extent,the carbonates control reservoir property and compressibility of muddy shale in the upper submember of Member 4 and lower submember of Member 3 of Shahejie Formation in Dongying sag,and provide important information for reconstruction of sedimentary environment of the ancient lake.

关键词： Formation mechanism Lacustrine facies Carbonate Muddy shale Shahejie formation Dongying sag

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Genesis of the high gamma sandstone of the Yanchang Formation in the Ordos Basin,China

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Petroleum Science 2013年第1期10卷 50-54页

作者： Liu Huaqing Li Xiangbo Liao Jianbo Liu Xianyang research institute of Petroleum exploration and development-Northwest research institute of exploration and development Changqing Oilfield Company

Recently, more attention has been paid on the high gamma sandstone reservoirs of the Yanchang Formation in the Ordos Basin, China. These high gamma sandstones have logging characteristics different from conventional sandstones, which influences the identification of sandstone reservoirs. Zhang et al （2010） proposed that the high gamma sandstones of the Yanchang Formation might be the result of re-deposition of homochronous sedimentary tufts or previous tufts as a part of the sandstone. However, we present a different viewpoint： 1） few tufts or tuff debris have been found in the high gamma sandstones of the Yanchang Formation; 2） high gamma （or high Th content） sandstones of Yanchang Formation are not related to either clay minerals or feldspar; 3） the heavy minerals in the sandstone reservoirs of the Yanchang Formation are dominated by zircon, which is characterized by abnormally high Th and U contents, up to 2,163 ppm and 1,362 ppm, respectively. This is sufficient to explain the high gamma anomaly. The conclusion is that the high gamma value of the Yanchang Formation sandstones might be caused by zircon with high Th and U contents in sandstones rather than from the tuff components.

关键词： High gamma sandstones reservoir zircon Yanchang Formation Ordos Basin

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Geological features and hydrocarbon accumulation in the Xinken oil field,Tarim Basin

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Chinese Journal Of Geochemistry 2013年第4期32卷 367-379页

作者： SONG Lichen ZHU Guangyou LIU Xingwang ZHU Yongfeng SU Jin WANG Kai research institute of Petroleum exploration and development PetroChina research institute of Petroleum exploration and development Tarim Oilfield CompanyPetroChina

Recently,a large-scale Ordovician oil and gas pool has been discovered in Xinken,north of the Tarim Basin,and it has strongly heterogeneous reservoirs and complicated fluid *** analyzing oil,gas and water samples collected from this area,in combination of field production and testing data,this study reveals that the Xinken oil pool contains dominantly normal oil characterized by low viscosity,low sulphur,and high *** has a low content of natural gas,which presents typical characteristics of wet gas and is oil-associated ***-gas correlation shows that the oil was from the Middle-Upper Ordovician source rocks and the charge and accumulation of oil and gas took place in the Late Hercynian *** by paleogeomorphology,sedimentary facies,ancient karstification,faults,and other factors in the Caledonian Period,the Ordovician carbonate reservoirs are dominated by dissolved pores,cavities and *** reservoir body of fractures and cavities is distributed in the shape of strip and laminate along faults and excellent reservoirs are mostly in the range of 70–100 m below the top of the Yijianfang *** a whole,the Xinken oil pool is a fracture-cavity pool controlled by interbedded karst reservoirs and is a complex composed of stacked karst fractures and cavities of various *** contains oil in large areas horizontally,which is quasi-laminated in distribution,and the accumulation of oil and gas is controlled by the distribution and development degree of the Ordovician carbonate *** study shows that this area has abundant resources and a great exploration potential for oil and gas.

关键词：塔里木盆地北部油气成藏地质特征碳酸盐岩储层石油伴生气油田储层控制非均质储层

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Evidence of the Near-Source Accumulation of the Tight Sandstone Gas in Northern Ordos Basin,North-Central China

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Acta Geologica Sinica(English Edition) 2017年第5期91卷 1820-1835页

作者： YANG Zhi LI Qiyan WU Songtao LIN Senhu LIU Xinshen research institute of Petroleum exploration & development Petro China research institute of exploration and development Petro China Changqing Oilfield Company

The tight sandstone gas in Upper Paleozoic Formation of the northern Ordos Basin is a typical giant unconventional tight gas province. Evidences from geochemistry, reservoir geology and paleotectonic setting all verify that the present-day tight sandstone gas accumulation in the Ordos Basin is the result of near-source accumulation. The evidences are listed as following： tight sandstone gas is mainly distributed in the area with high gas-generating strength; gas composition was not subjected tofractionation; gas saturation significantly decreases with the distance away from the source rocks; gas isotopes suggest their origin is the same and maturity is consistent with in-place source rocks; reservoirs have experienced three types of densification digenesis, including intense compaction, siliceous cementation and calcareous cementation, which took place before the formation of a large amount of tight sandstone gas, forming tight reservoirs with low porosity and permeability, fine pore throat and great capillary resistance; the paleo-structural gradient ratio is small from the main hydrocarbon generation period to present. It is indicated the present distribution of tight sandstone gas in the northern Ordos Basin is the result of near-source and short-distance migration and accumulation.

关键词： near-source accumulation tight sandstone gas coal measures unconventional gas geochemistry

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Re-Examination of the Oil and Gas Origins in the Kekeya Gas Condensate Field,Northwest China——A Case Study of Hydrocarbon-Source Correlation Using Sophisticated Geochemical Methods

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Acta Geologica Sinica(English Edition) 2017年第1期91卷 186-203页

作者： GONG Deyu WANG Zhaoyun LIU Gang CHEN Gang FANG Chenchen XIAO Zhongyao research institute of Petroleum exploration and development PetroChina Tarim oilfield company PetroChina

This work discussed the origins, alteration and accumulation processes of the oil and gas in the Kekeya gas condensate field based on molecular compositions, stable carbon isotopes, light hydrocarbons, diamondoid hydrocarbons and biomarker fingerprints. A comparison study is also made between the geochemical characteristics of the Kekeya hydrocarbons and typical marine and terrigenous hydrocarbons of the Tarim Basin. Natural gas from the Kekeya gas condensate field is derived from Middle–Lower Jurassic coal measures while the condensates are derived from Carboniferous–Permian marine source rocks with a higher maturity. In the study area, both natural gas and condensates have experienced severe water washing. A large amount of methane was dissolved into the water, resulting in a decrease in the dryness coefficient. Water washing also makes the carbon isotopic compositions of the natural gas more negative and partially reverse. Considering that the gas maturities are higher than once expected, gas generation intensity in the study area should be much stronger and the gas related to the Jurassic coal measures could promise a greater prospecting potential. As a result of evaporative fractionation, the Kekeya condensates are enriched in saturates and lack aromatics. Evaporative fractionation disguises the original terrigenous characteristics of the light hydrocarbons associated with the natural gas, making it appear marinesourced. Thus, alteration processes should be fully taken into consideration when gas–source correlations are carried out based on light hydrocarbons. With the condensates discovered in the study area all being ＂migration phase＂, the pre-salt Cretaceous and Jurassic reservoirs may promise great exploration potential for the ＂residual phase＂ hydrocarbons. This research not only is of significance for oil and gas exploration in the southwest Tarim Basin, but also sheds light on the oil/gas-source correlations in general.

关键词： Kekeya gas condensate field evaporative fractionation water washing coal-derived gas marine condensates stable carbon isotopes diamondoid hydrocarbons

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Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression,Tarim Basin,China

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Science China Earth Sciences 2008年第S1期51卷 195-206页

作者： LU YuHong,XIAO ZhongYao,GU QiaoYuan&ZHANG QiuCha research institute of exploration and development,Tarim oilfield company,PetroChina,Korla 841000,China research institute of exploration and development Tarim Oilfield Company PetroChina Korla China

There exists a petroleum system rich of oil and gas around Halahatang depression,where the oil and gas possess obvious local distinctions of properties in different *** research proved that the discovered crude oil and natural gas in the region derived mainly from O2+3 source rock,and the differences of its properties were controlled by the oil and gas filling *** comprehensive study result shows the oil and gas reservoirs of the region mainly underwent three important accumulation phases:late Caledonian-Early Hercynian epoch,late Hercynian epoch,and Yanshan-Himalayan epoch. In the first phase,the oil and gas derived mostly from Cambrian source rock,which formed the primary ancient oil reservoirs,then suffered strong degradation and remained a great quantity of pyrobitumen in the high position of Tabei uplift in the *** the second phase,the O2+3 source rock of Manjia'er depression started its generation of hydrocarbon,which accumulated in the high position of Tabei uplift afterwards,and then biodegradated to heavy oil in the late Hercynian *** the last phase,the O2+3 source rock of southern Halahatang depression and margin of Manjia'er depression started its peak of generating liquid hydrocarbon,which mostly accumulated in the trap formed before the Indo-China and Yanshan epoch,and in somewhere the heavy oil suffered dilutions in various degrees or serious gas invading,to lead to obvious crude oil divergence.

关键词： marine facies Mid-Upper Ordovician source rock oil and gas source accumulation stage Halahatang depression Tarim Basin

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Formation conditions and reservoir-forming models of the Ordovician buried hill reservoirs in the Jizhong depression

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地学前缘 2023年第1期30卷 229-241页

作者： ZHANG Ruifeng TIAN Jianzhang HUANG Yuanxin TIAN Ran REN Yi BIAN Yingying WANG Yuanjie CHEN Ling LU Shan PetroChina Huabei oilfield company Renqiu 062552China exploration and development research institute of PetroChina Huabei oilfield company Renqiu 062552China

The buried hill in the Jizhong depression contains abundant petroleum reserves and are important production *** Ordovician buried hill has restricted the discovery of new oil and gas exploration targets because of its strong reservoir heterogeneity and complex reservoir-controlling *** on a large volume of core,thin section,logging,seismic,and geochemical data and numerous geological analyses,the reservoir-forming conditions and modes were systematically analyzed to guide the exploration and achieve important breakthroughs in the Yangshuiwu and Wen an slope buried *** study revealed that three sets of source rocks of the third and fourth members of the Shahejie Formation from the Paleogene and Carboniferous-Permian were developed in the Jizhong depression,providing sufficient material basis for the formation of buried hill oil and gas *** reservoir control mechanism involving the three major factors of“cloud-karst-fault”was clarified,and karst cave,fracture fissure-pore,and cloud pore type reservoir models were established,thereby expanding the exploration *** by the superposition of multi-stage tectonic processes during the Indosinian,Yanshanian,and Himalayan,two genetic buried hill trap types of uplift-depression and depression-uplift were *** on the analysis of reservoir-forming factors of the Ordovician buried hill,three buried hill oil and gas reservoir-forming models were identified:low-level tectonic-lithologic composite quasi-layered buried hill,medium-level paleo-storage paleo-block buried hill,and high-level paleo-storage new-block buried *** evaluations indicate that the reservoir-forming conditions of the low-level tectonic-lithologic composite quasi-layered buried hill in the northern portion of the Jizhong depression are the most favorable and that the Sicundian and Xinzhen buried hills are favorable areas for future exploration.

关键词： Jizhong depression Yangshuiwu Ordovician reservoir type reservoir model

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Detrital Zircon U-Pb Dating for Clastic Rocks from Boreholes in the Eastern Junggar Basin:Constraints on Permian Tectonics in the Southern Central Asian Orogenic Belt

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Acta Geologica Sinica(English Edition) 2024年第6期98卷 1429-1440页

作者： REN Xincheng ZHANG Guanlong WANG Jinduo ZHANG Kuihua ZHANG Xuecai JI Ma YU Hongzhou exploration and development research institute Shengli Oilfield CompanySINOPECDongyingShandong 257015China Oil and Gas exploration and Management Center Shengli Oilfield CompanySINOPECDongyingShandong 257001China

Permian sedimentary successions,widely distributed in the eastern Junggar Basin,may record key details on the closure of the Paleo-Asian Ocean in this *** of boreholes show that Permian strata is mainly composed of mudstone,sandy mudstone,siltstone,sandstone,sandy conglomerate,dolomite,and *** zircon U-Pb dating results of three sandstone samples yielded the calculated maximum ages of 296 Ma,278 Ma and 293 Ma,indicating they possibly deposited during the Early *** strata in the eastern Junggar Basin show similar rock associations and detrital zircon age data distribution *** new and compiled age data for sandstone samples in the eastern Junggar Basin and Bogda region yield predominant Paleozoic ages,close to their sedimentary *** detrital zircon age data distribution patterns support the hypothesis that these Early Permian meta-clastic rocks in the eastern Junggar Basin and Bogda region were deposited in a subduction-related basin,and indicate an Early Permian Ocean prevented Precambrian detritus from the Central Tianshan block from depositing in the eastern Junggar Basin and Bogda region.

关键词： detrital zircon U-Pb dating tectonostratigraphy Junggar Basin Paleo-Asian Ocean

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