Based on new high-resolution seismic profiles and existing structural and sedimentary results,a superposition de-formation model for Cenozoic Bachu Uplift of northwestern Tarim Basin,northwestern China is proposed. Th...Based on new high-resolution seismic profiles and existing structural and sedimentary results,a superposition de-formation model for Cenozoic Bachu Uplift of northwestern Tarim Basin,northwestern China is proposed. The model presents the idea that the Bachu Uplift suffered structure superposition deformation under the dual influences of the Cenozoic uplifting of Southern Tianshan and Western Kunlun orogen,northwestern China. In the end of the Eocene (early Himalayan movement),Bachu Uplift started to be formed with the uplifting of Western Kunlun,and extended NNW into the interior of Kalpin Uplift. In the end of the Miocene (middle Himalayan movement),Bachu Uplift suffered not only the NNW structure deformation caused by the Western Kunlun uplifting,but also the NE structure deformation caused by the Southern Tianshan uplifting,and the thrust front fault of Kalpin thrust system related to the Southern Tianshan orogen intrudes southeastward into the hinterland of Bachu Uplift and extends NNE from well Pi1 to Xiaohaizi reservoir and Gudongshan mountain,which resulted in the strata folded and denuded strongly. In the end of the Pliocene (late Himalayan movement),the impact of Southern Tianshan orogen decreased because of the stress released with the breakthrough upward of Kalpin fault extending NE,and Bachu Uplift suffered mainly the structure deformation extending NW-NNW caused by the uplifting of Western Kunlun orogen.展开更多
Based on high-resolution 2D seismic profiles,the Paleozoic structural deformation char-acteristics of Bachu (巴楚) uplift of northwestern Tarim basin,NW China,are exhibited in this article. The deformation happened du...Based on high-resolution 2D seismic profiles,the Paleozoic structural deformation char-acteristics of Bachu (巴楚) uplift of northwestern Tarim basin,NW China,are exhibited in this article. The deformation happened during three main geological periods:the end of Middle-Late Ordovician (O2-3),the end of Early-Middle Devonian (D1-2),and the end of Late Permian (P2). In the Bachu uplift,there developed a series of NW-trending thrust faults and imbricate structures due to the effect of the NW-SE compression stress towards the end of Middle-Late Ordovician (O2-3) (middle Caledonian movement),and there developed some NNE-trending thrust faults and fault blocks under the control of the NEE-SWW compression stress at the end of Early-Middle Devonian (D1-2) (early Hercynian movement). However,at the end of Late Permian (P2) (late Hercynian movement),some NE-trending thrust faults and associated folds developed as a result of the NE-SW compression stress. The first-stage (O2-3) deformation is obviously more violent than those of the latter two stages (D1-2and P2),which implies that the Tarim plate drifted quickly to the north at around the same time basin.展开更多
The Bachu(巴楚) uplift is one of the most active tectonic regions nowadays in the Tarim basin,which is also a faulted block uplift that was intensively active during the Cenozoic.This study was based primarily on the ...The Bachu(巴楚) uplift is one of the most active tectonic regions nowadays in the Tarim basin,which is also a faulted block uplift that was intensively active during the Cenozoic.This study was based primarily on the geological structure interpretation of seismic profiles,applying the theories and methods of basin dynamics,structural analysis and tectono-stratigraphic analysis,the geometry and kinematics features of the fault systems in the Bachu uplift were analyzed in detail.Our study shows that each fault belt is mainly characterized by compression and overthrusting,most of the faults initiated and activated during the Mid-Late Himalayan period,and that the general structural styles of the Bachu uplift were basement-involved pop-up thrust faulted block uplift,of which the southern margin was covered by the large-scale decollement fault system.The basement-involved structures widely developed in the higher position of the basement uplift,while decollement fault system developed mainly at the position with gypsum mudstone.The evolution process of Bachu uplift included back-bulge slope of the peripheral foreland basin in Mid-Late Caledonian,forebulge in Hercynian-Yanshanian and the latest compressional faulted block uplift in Mid-Late Himalayan.Meanwhile,the study also suggests that the formation,reconstruction and stabilization of the uplift were controlled by the development and evolution of fault systems clearly.In the early forebulge stage,it was mainly presented as flexural deformation without the developing of thrust faults in the Bachu area;to the late stage,under the influence of violent lateral compression deformation,the faulted block uplift formed finally.展开更多
基金Project supported by the National Science and Technology Project of Tenth Five Years (No.2001BA605A06A)Science and Tech-nology Cooperation Program of SINOPEC (No.FYWX04-06),China
文摘Based on new high-resolution seismic profiles and existing structural and sedimentary results,a superposition de-formation model for Cenozoic Bachu Uplift of northwestern Tarim Basin,northwestern China is proposed. The model presents the idea that the Bachu Uplift suffered structure superposition deformation under the dual influences of the Cenozoic uplifting of Southern Tianshan and Western Kunlun orogen,northwestern China. In the end of the Eocene (early Himalayan movement),Bachu Uplift started to be formed with the uplifting of Western Kunlun,and extended NNW into the interior of Kalpin Uplift. In the end of the Miocene (middle Himalayan movement),Bachu Uplift suffered not only the NNW structure deformation caused by the Western Kunlun uplifting,but also the NE structure deformation caused by the Southern Tianshan uplifting,and the thrust front fault of Kalpin thrust system related to the Southern Tianshan orogen intrudes southeastward into the hinterland of Bachu Uplift and extends NNE from well Pi1 to Xiaohaizi reservoir and Gudongshan mountain,which resulted in the strata folded and denuded strongly. In the end of the Pliocene (late Himalayan movement),the impact of Southern Tianshan orogen decreased because of the stress released with the breakthrough upward of Kalpin fault extending NE,and Bachu Uplift suffered mainly the structure deformation extending NW-NNW caused by the uplifting of Western Kunlun orogen.
基金The National Major Fundamental Research and Development Project(2005CB422102)Notional Key Project for Oil and Gas(2008ZX05007-03)Key Project of SINOPEC provided financial support for this work
基金supported by the National Science and Technology Project of Tenth Five Years (No. 2001BA605A06A)Science and the Technology Cooperation Programs of SINOPEC, China (Nos. FYWX04-06, XBKT2007KY10-021)
文摘Based on high-resolution 2D seismic profiles,the Paleozoic structural deformation char-acteristics of Bachu (巴楚) uplift of northwestern Tarim basin,NW China,are exhibited in this article. The deformation happened during three main geological periods:the end of Middle-Late Ordovician (O2-3),the end of Early-Middle Devonian (D1-2),and the end of Late Permian (P2). In the Bachu uplift,there developed a series of NW-trending thrust faults and imbricate structures due to the effect of the NW-SE compression stress towards the end of Middle-Late Ordovician (O2-3) (middle Caledonian movement),and there developed some NNE-trending thrust faults and fault blocks under the control of the NEE-SWW compression stress at the end of Early-Middle Devonian (D1-2) (early Hercynian movement). However,at the end of Late Permian (P2) (late Hercynian movement),some NE-trending thrust faults and associated folds developed as a result of the NE-SW compression stress. The first-stage (O2-3) deformation is obviously more violent than those of the latter two stages (D1-2and P2),which implies that the Tarim plate drifted quickly to the north at around the same time basin.
基金supported by the National Science and Technology Major Project (No. 2011ZX05009-001)the National Natural Science Foundation of China (No. 41102071)
文摘The Bachu(巴楚) uplift is one of the most active tectonic regions nowadays in the Tarim basin,which is also a faulted block uplift that was intensively active during the Cenozoic.This study was based primarily on the geological structure interpretation of seismic profiles,applying the theories and methods of basin dynamics,structural analysis and tectono-stratigraphic analysis,the geometry and kinematics features of the fault systems in the Bachu uplift were analyzed in detail.Our study shows that each fault belt is mainly characterized by compression and overthrusting,most of the faults initiated and activated during the Mid-Late Himalayan period,and that the general structural styles of the Bachu uplift were basement-involved pop-up thrust faulted block uplift,of which the southern margin was covered by the large-scale decollement fault system.The basement-involved structures widely developed in the higher position of the basement uplift,while decollement fault system developed mainly at the position with gypsum mudstone.The evolution process of Bachu uplift included back-bulge slope of the peripheral foreland basin in Mid-Late Caledonian,forebulge in Hercynian-Yanshanian and the latest compressional faulted block uplift in Mid-Late Himalayan.Meanwhile,the study also suggests that the formation,reconstruction and stabilization of the uplift were controlled by the development and evolution of fault systems clearly.In the early forebulge stage,it was mainly presented as flexural deformation without the developing of thrust faults in the Bachu area;to the late stage,under the influence of violent lateral compression deformation,the faulted block uplift formed finally.
