Effect of thermochemical sulfate reduction on carbonate reservoir quality: Cambrian and Ordovician oilfield, Tazhong area, Tarim basin, China

[1]  Anjiang Shen,et al.  Reservoir geological modeling and significance of Cambrian Xiaoerblak Formation in Keping outcrop area, Tarim Basin, NW China , 2020, Petroleum Exploration and Development.

[2]  Yang Pengfei,et al.  Great discovery and its significance of ultra-deep oil and gas exploration in well Luntan-1 of the Tarim Basin , 2020 .

[3]  V. Lüders,et al.  Fluid inclusion evidence for low-temperature thermochemical sulfate reduction (TSR) of dry coal gas in Upper Permian carbonate reservoirs (Zechstein, Ca2) in the North German Basin , 2020 .

[4]  Tongwei Zhang,et al.  Kinetics of elemental sulfur reduction by petroleum hydrocarbons and the implications for hydrocarbon thermal chemical alteration , 2019, Geochimica et Cosmochimica Acta.

[5]  V. Lüders,et al.  Super-deep, TSR-controlled Phanerozoic MVT type Zn-Pb deposits hosted by Zechstein-2 gas reservoir carbonate (Ca2), Lower Saxony Basin, Germany , 2019, Chemical Geology.

[6]  Xuefeng Zhang,et al.  Fluid inclusion and stable isotopic studies of thermochemical sulfate reduction: Upper permian and lower triassic gasfields, northeast Sichuan Basin, China , 2019, Geochimica et Cosmochimica Acta.

[7]  Changbing Yang,et al.  Thermochemical sulphate reduction can improve carbonate petroleum reservoir quality , 2018 .

[8]  C. Cai,et al.  The Effect of Water Chemistry on Thermochemical Sulfate Reduction: A Case Study from the Ordovician in the Tazhong Area, Northwest China , 2017 .

[9]  Lei Jiang,et al.  Petrological and geochemical constraints on diagenesis and deep burial dissolution of the Ordovician carbonate reservoirs in the Tazhong area, Tarim Basin, NW China , 2016 .

[10]  P. Mei,et al.  Pyrite‐hydrocarbon Interaction under Hydrothermal Conditions: an Alternative Origin of H2S and Organic Sulfur Compounds in Sedimentary Environments , 2016 .

[11]  R. H. Worden,et al.  Multiphase dolomitization of deeply buried Cambrian petroleum reservoirs, Tarim Basin, north‐west China , 2016 .

[12]  Dianwei Zhang,et al.  Coupled alteration of hydrothermal fluids and thermal sulfate reduction (TSR) in ancient dolomite reservoirs – An example from Sinian Dengying Formation in Sichuan Basin, southern China , 2016 .

[13]  Xiaomei Wang,et al.  New insights into the formation mechanism of high hydrogen sulfide–bearing gas condensates: Case study of Lower Ordovician dolomite reservoirs in the Tazhong uplift, Tarim Basin , 2016 .

[14]  C. Cai,et al.  Sulfur isotopic compositions of individual organosulfur compounds and their genetic links in the Lower Paleozoic petroleum pools of the Tarim Basin, NW China , 2016 .

[15]  P. Kukla,et al.  Impacts of hydrothermal dolomitization and thermochemical sulfate reduction on secondary porosity creation in deeply buried carbonates: A case study from the Lower Saxony Basin, northwest Germany , 2016 .

[16]  Xiaomei Wang,et al.  Genetic origin of sour gas condensates in the Paleozoic dolomite reservoirs of the Tazhong Uplift, Tarim Basin , 2015 .

[17]  Baoshou Zhang,et al.  Origins and fates of H2S in the Cambrian and Ordovician in Tazhong area: Evidence from sulfur isotopes, fluid inclusions and production data , 2015 .

[18]  R. H. Worden,et al.  Generation of isotopically and compositionally distinct water during thermochemical sulfate reduction (TSR) in carbonate reservoirs: Triassic Feixianguan Formation, Sichuan Basin, China , 2015 .

[19]  Baoshou Zhang,et al.  Thermochemical and bacterial sulfate reduction in the Cambrian and Lower Ordovician carbonates in the Tazhong Area, Tarim Basin, NW China: evidence from fluid inclusions, C, S, and Sr isotopic data , 2015 .

[20]  Zaixing Jiang,et al.  The role of thermochemical sulfate reduction in the genesis of high-quality deep marine reservoirs within the central Tarim Basin, western China , 2015, Arabian Journal of Geosciences.

[21]  Richard H. Worden,et al.  Enrichment of nitrogen and 13C of methane in natural gases from the Khuff Formation, Saudi Arabia, caused by thermochemical sulfate reduction , 2015 .

[22]  Guangwei Wang,et al.  Heterogeneous distribution of pyrobitumen attributable to oil cracking and its effect on carbonate reservoirs: Feixianguan Formation in the Jiannan gas field, China , 2015 .

[23]  Xuefeng Zhang,et al.  The fate of CO2 derived from thermochemical sulfate reduction (TSR) and effect of TSR on carbonate porosity and permeability, Sichuan Basin, China , 2015 .

[24]  Zhaoming Wang,et al.  Origin of late charged gas and its effect on property of oils in the Ordovician in Tazhong area , 2014 .

[25]  Lei Jiang,et al.  Petrological and geochemical constraints on porosity difference between Lower Triassic sour- and sweet-gas carbonate reservoirs in the Sichuan Basin , 2014 .

[26]  Wenzhi Zhao,et al.  The porosity origin of dolostone reservoirs in the Tarim, Sichuan and Ordos basins and its implication to reservoir prediction , 2014, Science China Earth Sciences.

[27]  C. Yang,et al.  Thermochemical sulphate reduction (TSR) versus maturation and their effects on hydrogen stable isotopes of very dry alkane gases , 2014 .

[28]  R. H. Worden,et al.  Thermochemical sulfate reduction and fluid evolution of the Lower Triassic Feixianguan Formation sour gas reservoirs, northeast Sichuan Basin, China , 2014 .

[29]  Hong He,et al.  Carbon isotope fractionation during methane-dominated TSR in East Sichuan Basin gasfields, China: A review , 2013 .

[30]  Daizhao Chen,et al.  Hydrothermal alteration of dolostones in the Lower Ordovician, Tarim Basin, NW China: Multiple constraints from petrology, isotope geochemistry and fluid inclusion microthermometry , 2013 .

[31]  K. Bjørlykke,et al.  Open or closed geochemical systems during diagenesis in sedimentary basins: Constraints on mass transfer during diagenesis and the prediction of porosity in sandstone and carbonate reservoirs , 2012 .

[32]  Tongwei Zhang,et al.  Kinetics of uncatalyzed thermochemical sulfate reduction by sulfur-free paraffin , 2012 .

[33]  X. Pang,et al.  Origin of the unusually high dibenzothiophene oils in Tazhong-4 Oilfield of Tarim Basin and its implication in deep petroleum exploration , 2012 .

[34]  N. Qiu,et al.  Thermal evolution and maturation of lower Paleozoic source rocks in the Tarim Basin, northwest China , 2012 .

[35]  T. Bolin,et al.  Thermal transformations of organic and inorganic sulfur in Type II kerogen quantified by S-XANES , 2012 .

[36]  Yongfeng Zhu,et al.  Distribution and erosion of the Paleozoic tectonic unconformities in the Tarim Basin, Northwest China: Significance for the evolution of paleo-uplifts and tectonic geography during deformation , 2012 .

[37]  P. Mankiewicz,et al.  Thiadiamondoids as proxies for the extent of thermochemical sulfate reduction , 2012 .

[38]  K. Bjørlykke,et al.  Carbonate porosity creation by mesogenetic dissolution: Reality or illusion? , 2012 .

[39]  T. Bolin,et al.  Characterization of solid bitumens originating from thermal chemical alteration and thermochemical sulfate reduction , 2010 .

[40]  Lei Xiang,et al.  TSR origin of sulfur in Permian and Triassic reservoir bitumen, East Sichuan Basin, China , 2010 .

[41]  X. Pang,et al.  Petroleum source in the Tazhong Uplift, Tarim Basin: New insights from geochemical and fluid inclusion data , 2010 .

[42]  B. Onac,et al.  Sulfur isotopic composition and the source of dissolved sulfur species in thermo-mineral springs of the Cerna Valley, Romania , 2010 .

[43]  R. Swennen,et al.  Host rock dolomitization and secondary porosity development in the Upper Devonian Cairn Formation of the Fairholme carbonate complex (South‐west Alberta, Canadian Rockies): diagenesis and geochemical modelling , 2009 .

[44]  Lei Jiang,et al.  Origins of Palaeozoic oils in the Tarim Basin: Evidence from sulfur isotopes and biomarkers , 2009 .

[45]  Shuichang Zhang,et al.  Relationship between the later strong gas-charging and the improvement of the reservoir capacity in deep Ordovician carbonate reservoir in Tazhong area, Tarim Basin , 2009 .

[46]  R. H. Worden,et al.  Distinguishing Cambrian from Upper Ordovician source rocks: Evidence from sulfur isotopes and biomarkers in the Tarim Basin , 2009 .

[47]  Baoshou Zhang,et al.  Evidence for cross formational hot brine flow from integrated 87Sr/86Sr, REE and fluid inclusions of the Ordovician veins in Central Tarim, China , 2008 .

[48]  Tongwei Zhang,et al.  Experimental investigation on thermochemical sulfate reduction by H2S initiation , 2008 .

[49]  B. Taylor,et al.  Sulfur Isotope Evidence for Thermochemical Reduction of Dissolved Sulfate in Mississippi Valley-Type Zinc-Lead Mineralization, Bongara Area, Northern Peru , 2008 .

[50]  B. E. Buschkuehle,et al.  Diagenesis of the Devonian Southesk-Cairn Carbonate Complex, Alberta, Canada: Marine Cementation, Burial Dolomitization, Thermochemical Sulfate Reduction, Anhydritization, and Squeegee Fluid Flow , 2008 .

[51]  T. Guo,et al.  Evidence for multiple stages of oil cracking and thermochemical sulfate reduction in the Puguang gas field, Sichuan Basin, China , 2008 .

[52]  He Jiang,et al.  Unique optimal solution instance and computational complexity of backbone in the graph bi-partitioning problem , 2007 .

[53]  Qilai Xie,et al.  The Silurian play in the Tazhong Uplift, Tarim Basin, northwestern China , 2007 .

[54]  G. Davies,et al.  Structurally controlled hydrothermal dolomite reservoir facies: An overview , 2006 .

[55]  Jiamo Fu,et al.  Chemical and carbon isotopic fractionations of gaseous hydrocarbons during abiogenic oxidation , 2006 .

[56]  S. Bottrell,et al.  Thermochemical sulphate reduction and the generation of hydrogen sulphide and thiols (mercaptans) in Triassic carbonate reservoirs from the Sichuan Basin, China , 2003 .

[57]  E. Brosse,et al.  Assessment of anhydrite dissolution as the rate-limiting step during thermochemical sulfate reduction , 2001 .

[58]  C. Cai,et al.  Thermochemical sulphate reduction in Cambro-Ordovician carbonates in Central Tarim , 2001 .

[59]  J. Alonso-Azcárate,et al.  Sulfur redox reactions and formation of native sulfur veins during low grade metamorphism of gypsum evaporites, Cameros Basin (NE Spain) , 2001 .

[60]  H. Machel.  Bacterial and thermochemical sulfate reduction in diagenetic settings — old and new insights , 2001 .

[61]  H. Krouse,et al.  Fluid Inclusion and Stable Isotopic Studies of Thermochemical Sulphate Reduction from Burnt Timber and Crossfield East Gas Fields in Alberta, Canada , 2001 .

[62]  M. Cross,et al.  The Influence of Rock Fabric and Mineralogy on Thermochemical Sulfate Reduction: Khuff Formation, Abu Dhabi , 2000 .

[63]  R. H. Worden,et al.  Gas Souring by Thermochemical Sulfate Reduction at 140¡C: Reply , 1997 .

[64]  Hanlin Chen,et al.  Geological thermal events in Tarim Basin , 1997 .

[65]  Richard H. Worden,et al.  H2S-producing reactions in deep carbonate gas reservoirs: Khuff Formation, Abu Dhabi , 1996 .

[66]  R. H. Worden,et al.  THE EFFECTS OF THERMOCHEMICAL SULFATE REDUCTION UPON FORMATION WATER SALINITY AND OXYGEN ISOTOPES IN CARBONATE GAS RESERVOIRS , 1996 .

[67]  R. Sassen,et al.  Products and distinguishing criteria of bacterial and thermochemical sulfate reduction , 1995 .

[68]  H. Krouse,et al.  Controls on the Origin and Distribution of Elemental Sulfur, H2S, and CO2in Paleozoic Hydrocarbon Reservoirs in Western Canada , 1995 .

[69]  E. Mountjoy,et al.  Origin of dissolution vugs, caverns, and breccias in the Middle Devonian Presqu'ile barrier, host of Pine Point mississippi valley-type deposits , 1994 .

[70]  M. L. Gorbaty,et al.  Transformation kinetics of organic sulphur forms in Argonne Premium coals during pyrolysis , 1993 .

[71]  R. Bodnar.  Revised equation and table for determining the freezing point depression of H2O-Nacl solutions , 1993 .

[72]  A. Ueda,et al.  Chemical and isotopic evidence of thermochemical sulphate reduction by light hydrocarbon gases in deep carbonate reservoirs , 1988, Nature.

[73]  Y. Druckman,et al.  Burial Diagenesis and Porosity Evolution, Upper Jurassic Smackover, Arkansas and Louisiana , 1981 .

[74]  Lei Jiang,et al.  Diagenesis of an evaporite-related carbonate reservoir in deeply buried Cambrian strata, Tarim Basin, northwest China , 2018 .

[75]  C. Cai,et al.  Origin and evolution of formation water from the Ordovician carbonate reservoir in the Tazhong area, Tarim Basin, NW China , 2017 .

[76]  X. Pang,et al.  Origin and quantitative source assessment of deep oils in the Tazhong Uplift, Tarim Basin , 2015 .

[77]  Zhaocui Wen.  Types and distributional features of Cambrian-Ordovician dolostone reservoirs in Tarim Basin,northwestern China , 2012 .

[78]  Chen Zhiyong,et al.  The tectonothermal events,architecture and evolution of Tarim craton basement palaeo-uplifts , 2012 .

[79]  Liang Yingbo.  Formation mechanism and distribution prediction of high-quality marine reservoir in deeper Sichuan Basin , 2006 .

[80]  Huang Hai-ping.  Oil accumulation history in Tadong 2 oil reservoir in Tarim Basin, NW China-A case study of oil stability and cracking , 2004 .

[81]  J. Menzies.  Microstructures in Diamictites of the Lower Gowganda Formation (Huronian), Near Elliot Lake, Ontario: Evidence for Deforming-Bed Conditions at the Grounding Line? , 2000 .

[82]  G. Barić,et al.  Petroleum geochemistry of the deep part of the Drava Depression, Croatia , 1998 .

[83]  E. Heydari.  The Role of Burial Diagenesis in Hydrocarbon Destruction and H2S Accumulation, Upper Jurassic Smackover Formation, Black Creek Field, Mississippi , 1997 .

[84]  R. H. Worden,et al.  Gas Souring by Thermochemical Sulfate Reduction at 140øC , 1995 .

[85]  R. Goldstein,et al.  Systematics of fluid inclusions in diagenetic minerals , 1994 .

[86]  H. Sakai,et al.  The age curves of sulfur and oxygen isotopes in marine sulfate and their mutual interpretation , 1980 .