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Origin and growth mechanisms of strike-slip faults in the central Tarim cratonic basin, NW China

Petroleum Exploration and Development 2021年第3期48卷 595-607页

作者： WU Guanghui MA Bingshan HAN Jianfa GUAN Baozhu CHEN Xin YANG Peng XIE Zhou School of Geoscience and Technology Southwest Petroleum UniversityChengdu 610500China PetroChina Key Laboratory of Carbonate Reservoir Southwest Petroleum UniversityChengdu 610500China Tarim Oilfield Company PetroChinaKorla 841000China State Key Laboratory of Continental Dynamics Northwest UniversityXi'an 710069China

Through fault structure analysis and chronology study, we discuss the origin and growth mechanisms of strike-slip faults in the Tarim Basin.(1) Multiple stages strike-slip faults with inherited growth were developed in the central Tarim cratonic basin. The faults initiation time is constrained at the end of Middle Ordovician of about 460 Ma according to U-Pb dating of the fault cements and seismic interpretation.(2) The formation of the strike-slip faults was controlled by the near N-S direction stress field caused by far-field compression of the closing of the Proto-Tethys Ocean.(3) The faults localization and characteristics were influenced by the pre-existing structures of the NE trending weakening zones in the basement and lithofacies change from south to north.(4) Following the fault initiation under the Andersonian mechanism, the strike-slip fault growth was dominantly fault linkage, associated with fault tip propagation and interaction of non-Andersonian mechanisms.(5) Sequential slip accommodated deformation in the conjugate strike-slip fault interaction zones, strong localization of the main displacement and deformation occurred in the overlap zones in the northern Tarim, while the fault tips, particularly of narrow-deep grabens, and strike-slip segments in thrust zones accumulated more deformation and strain in the Central uplift. In conclusion, non-Andersonian mechanisms, dominantly fault linkage and interaction, resulted in the small displacement but long intraplate strike-slip fault development in the central Tarim Basin. The regional and localized field stress, and pre-existing structures and lithofacies difference had strong impacts on the diversity of the strike-slip faults in the Tarim cratonic basin.

关键词： strike-slip fault fault dating fault growth mechanism non-Andersonian faulting stress field pre-existing structure Tarim Basin

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Nomore blind dates with calcite: Fluid-flow vs. fault-slip along the Očkov thrust, Prague Basin

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Geoscience Frontiers 2021年第4期12卷 163-174页

作者： Nick M.W.Roberts JiříŽák František Vacek JiříSláma Geochronology and Tracers Facility British Geological SurveyEnvironmental Science CentreNottingham NG125GGUK Institute of Geology and Paleontology Faculty of ScienceCharles UniversityAlbertov 6Prague 12843Czech Republic Department of Mineralogy and Petrology National MuseumVáclavskénáměstí68Prague 11579Czech Republic Institute of Geology Czech Academy of Sciencesv.v.i.Rozvojová269Prague 16500Czech Republic

dating of fracture-filling calcitewith U-Pb geochronology is becoming a rapidly adopted technique for determining the absolute timing of brittle deformation in the upper crust.Slickenfibre calcite is a desirable target,as it precipitates between individual fault slip displacement events,and provides additional kinematic information.Here we present a case study of slickenfibres formed on the Očkov thrust in the Lower Palaezoic Prague Basin,Bohemian Massif,utilising a combination of petrographic and in situ methods.We demonstrate that slickenfibre external textures can be preserved,whilst internally primary textures are removed by fluid infiltration and recrystallization,leading to variable U and Pb mobilisation.One slickenfibre yielded a date of ca.250 Ma,which we interpret as recording fault slip along the Očkov thrust.Another cross-cutting slickenfibre yielded more scattered U-Pb data,with an imprecise apparent age around ca.95 Ma.This slickenfibre is recrystallised,destroying the primary textures,and exhibits element mobility.The meaning of this younger apparent age is therefore questionable;whereas it likely reflects Cretaceous U and Pb mobility assisted by fluid-flow along the fault plane,it may not reflect a period of fault slip.Our results demonstrate that slickenfibre-based U-Pb dates do not unequivocally relate to fault motion,and that petrographic and elemental analyses are important requirements for interpreting calcite U-Pb data.

关键词： U-Pb geochronology Calcite fault dating Fluid-flow Prague Basin LA-ICP-MS

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No more blind dates with calcite:Fluid-flow vs.fault-slip along the O?kov thrust,Prague Basin

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Geoscience Frontiers 2021年第4期12卷 167-178页

作者： Nick M.W.Roberts Ji?í ?ák Franti?ek Vacek Ji?í Sláma Geochronology and Tracers Facility British Geological SurveyEnvironmental Science Centre Institute of Geology and Paleontology Faculty of ScienceCharles University Department of Mineralogy and Petrology National Museum Institute of Geology Czech Academy of Sciences

dating of fracture-filling calcite with U-Pb geochronology is becoming a rapidly adopted technique for determining the absolute timing of brittle deformation in the upper crust.Slickenfibre calcite is a desirable target,as it precipitates between individual fault slip displacement events,and provides additional kinematic information.Here we present a case study of slickenfibres formed on the O?kov thrust in the Lower Palaezoic Prague Basin,Bohemian Massif,utilising a combination of petrographic and in situ methods.We demonstrate that slickenfibre external textures can be preserved,whilst internally primary textures are removed by fluid infiltration and recrystallization,leading to variable U and Pb mobilisation.One slickenfibre yielded a date of ca.250 Ma,which we interpret as recording fault slip along the O?kov thrust.Another cross-cutting slickenfibre yielded more scattered U-Pb data,with an imprecise apparent age around ca.95 Ma.This slickenfibre is recrystallised,destroying the primary textures,and exhibits element mobility.The meaning of this younger apparent age is therefore questionable;whereas it likely reflects Cretaceous U and Pb mobility assisted by fluid-flow along the fault plane,it may not reflect a period of fault slip.Our results demonstrate that slickenfibre-based U-Pb dates do not unequivocally relate to fault motion,and that petrographic and elemental analyses are important requirements for interpreting calcite U-Pb data.

关键词： U-Pb geochronology Calcite fault dating Fluid-flow Prague Basin LA-ICP-MS

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