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Xixi Zhao - One of the best experts on this subject based on the ideXlab platform.
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Mesozoic tectonic evolution of the southeast china block new insights from basin analysis
Journal of Asian Earth Sciences, 2009Co-Authors: X M Zhou, Bo Wang, Xixi Zhao, P Deng, Shaoyong Jiang, Jinhai YuAbstract:Abstract In order to better understand the Mesozoic tectonic evolution of Southeast China Block (SECB in short), this paper describes geological features of Mesozoic basins that are widely distributed in the SECB. The analyzed data are derived from a regional geological investigation on various Mesozoic basins and a recently compiled 1:1,500,000 geological map of Mesozoic–Cenozoic basins. Two types of basin are distinguished according to their tectonic settings, namely, the post-orogenic basin (Type I) and the intracontinental extensional basin (Type II); the latter includes the graben and the half-graben or faulted-depression basins. Our studies suggest that the formation of these basins connects with the evolution of geotectonics of the SECB. The post-orogenic basin (Type I) was formed in areas from the piedmont to the intraland during the interval from Late Triassic to Early Jurassic; and the formation of the intracontinental extensional basin (Type II) connects with an intracontinental crustal thinning setting in the Late Mesozoic. The graben basin was generated during the Middle Jurassic and is associated with a bimodal volcanic eruption; and the half-graben or faulted-depression basin, filled mainly by the rhyolite, tuff and sedimentary rocks during Early Cretaceous, is occupied by the Late Cretaceous–Paleogene red-colored terrestrial clastic rocks. We noticed that the modern outcrops of numerous granites and basins occur in a similar level, and the Mesozoic granitic bodies contact with the adjacent basins by large normal faults, suggesting that the modern landforms between granites and basins were yielded by the late crustal movement. The modern basin and range framework was settled down in the Cretaceous. Abundant sedimentary structures are found in the various basins, from that the deposited environments and paleo-currents are concluded; during the Late Triassic–Early Jurassic time, the source areas were situated to the north and northeast sides of the outcrop region. In this paper, we present the study results on one geological and geographical separating unit and two separating fault zones. The Wuyi orogenic belt is a Late Mesozoic paleo-geographically separating unit, the Ganjiang fault zone behaves as the western boundary of Early Cretaceous volcanic rocks, and the Zhenghe–Dapu fault zone separates the SE-China Coastal Late Mesozoic volcanic-sedimentary basins and the Wuyi orogenic belt. Finally, we discuss the geodynamic mechanisms forming various basins, proposing a three-stage model of the Mesozoic sedimentary evolution.
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Isotopic and paleomagnetic constraints on the Mesozoic tectonic evolution of south China
Journal of Geophysical Research: Solid Earth, 1996Co-Authors: Stuart Gilder, James B. Gill, Robert S. Coe, Xixi Zhao, Zhongwei Liu, Genxian Wang, Kuirong Yuan, Wenlong Liu, Guodun KuangAbstract:In order to better constrain the paleogeographic evolution of south China we measured Sm-Nd and Rb-Sr isotopic compositions for 23 Mesozoic granites that crop out throughout the area. Tightly grouped neodymium depleted mantle model ages (1.4 ± 0.3 Ga) suggest the region is underlain by relatively homogeneous Proterozoic crust and fail to define crustal provinces. Neither the isotopic nor geologic data suggest that a Mesozoic suture exists. However, granites possessing anomalously high Sm (>8 ppm) and Nd (>45 ppm) concentrations, relatively high initial epsilon neodymium (−4 to −8), and high but variable initial 87Sr/86Sr (0.759 to 0.713) form a northeast trending zone that coincides with two prominent Mesozoic basins. Southeast of the zone lie the majority of Mesozoic intrusives and Upper Triassic to Lower Cretaceous extensional basins found in south China. Mesozoic paleomagnetic poles are well clustered northwest of the zone. Pre-Cretaceous poles southeast of it are discordant with respect to those from the northwest. The only recognized tectonostratigraphic terrane in south China lies southeast of the zone. The terrane is bordered by a northeast trending sinistral fault that was active in the Mesozoic. Other faults in south China have similar attitudes, ages, and sense of shear. Together, the observations suggest that the Mesozoic tectonic regime in south China consisted of strike-slip activity plus concomitant rifting as terranes or fragments of similar crust were transported north along sinistral faults. The zone, defined by the granites enriched in Nd and Sm, demarcates displaced terranes to the southeast from relatively stable land to the northwest.
M Santosh - One of the best experts on this subject based on the ideXlab platform.
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a Mesozoic orogenic cycle from post collision to subduction in the southwestern korean peninsula new structural geochemical and chronological evidence
Journal of Asian Earth Sciences, 2017Co-Authors: Seung Ik Park, Sanghoon Kwon, Paul S Hong, M SantoshAbstract:Abstract The Early to Middle Mesozoic basins, distributed sporadically over the Korean Peninsula, preserve important records of the tectonic history of some of the major orogenic belts in East Asia. Here we present a comprehensive study of the structural, geochemical, geochronological, and paleontological features of a volcano-sedimentary package, belonging to the Oseosan Volcanic Complex of the Early to Middle Mesozoic Chungnam Basin, within the Mesozoic subduction-collision orogen in the southwestern Korean Peninsula. The zircon U-Pb data from rhyolitic volcanic rocks of the complex suggest Early to Middle Jurassic emplacement age of ca. 178–172 Ma, harmonious with plant fossil taxa found from the overlying tuffaceous sedimentary rock. The geochemical data for the rhyolitic volcanic rocks are indicative of volcanic arc setting, implying that the Chungnam Basin has experienced an intra-arc subsidence during the basin-expanding stage by subduction of the Paleo-Pacific (Izanagi) Plate. The Jurassic arc-related Oseosan Volcanic Complex was structurally stacked by the older Late Triassic to Early Jurassic post-collisional basin-fill of the Nampo Group by the Jangsan fault during basin inversion. The Late Jurassic to Early Cretaceous K-feldspar and illite K-Ar ages marked the timing of inversion tectonics, contemporaneous with the magmatic quiescence in the southern Korean Peninsula, likely due to flat-lying or low-angle subduction. The basin evolution history preserved in the Mesozoic Chungnam Basin reflects a Mesozoic orogenic cycle from post-collision to subduction in the southwestern Korean Peninsula. This, in turn, provides a better understanding of the spatial and temporal changes in Mesozoic tectonic environments along the East Asian continental margin.
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Mesozoic basins in eastern china and their bearing on the deconstruction of the north china craton
Journal of Asian Earth Sciences, 2012Co-Authors: Guochun Zhao, M Santosh, Liming Dai, Xin Liu, Lihong Zhou, Yanhui SuoAbstract:Abstract Mesozoic basins occur widely in the Eastern Block and the neighboring area of the North China Craton, including the Bohai Bay, the Jiaolai, the Hefei and the North Yellow Sea in the north, and the Jianghan and the Subei-South Yellow Sea basins to the south. Their spatial–temporal framework is the consequence of the Indosinian and Yanshanian tectonic regimes in eastern China and record the events related to Mesozoic deconstruction of the North China Craton. Our results demonstrate that the Mesozoic tectonic evolution of the eastern North China Craton was related to both sub-crustal delamination and intra-crustal extrusion or escape tectonics. Thus, we propose that the mechanism of uplift of the Yanshanian North China Plateau and related lithosphere thinning in the eastern North China Craton were related to sub-crustal delamination at depth. However, the different distribution patterns of the basins on both sides of the Tan-Lu Fault System as well as the co-existence of both compressional and extensional basins in the Mesozoic indicate that these were controlled by escape tectonics in different tectonic parts of the crust.
Sheng Zhan - One of the best experts on this subject based on the ideXlab platform.
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Mesozoic magmatism and granitic dome in the Wugongshan Massif, Jiangxi province and their genetical relationship to the tectonic events in southeast China
Tectonophysics, 2001Co-Authors: D.z. Wang, Liangshu S. Shu, Michel Faure, Sheng ZhanAbstract:In SE China, a Mesozoic granitic dome coeval to extensional tectonics is exposed in the Wugongshan massif. Its center is occupied by Mesozoic granitoids and granitic gneisses, and the E–W-trending Late-Paleozoic–Mesozoic Pingxiang and Anfu basins are located along its northern and southern sides, respectively. In this paper, the petrological, geochemical (major, incompatible, and rare earth elements) and isotopic characteristics of the granitoids and granitic gneisses of this dome allow us to constrain their geodynamic evolution. The Wugongshan Mesozoic K-feldspar-enriched granitoids consist of six granitic bodies and lie within a Paleozoic metamorphic basement. The Caledonian Shanzhuang granodiorite, containing some dioritic enclaves, occurs in the study area and is a calc-alkaline type granodiorite characterised by lower SiO2 and composed of andesine, biotite, quartz, hornblende, magnetite and sphene. The Mesozoic granitoids, either Indosinian plutons or Yanshanian bodies, show a geochemical affinity of peraluminous S-type granite, having higher SiO2, K2O contents, Al>K+Na+2Ca, enriched in Rb, Th and depleted in Eu. They also exhibit LREE-enriched patterns and marked negative Eu anomalies. The Yanshanian plutons also contain characteristic minerals such as sillimanite, garnet and monazite. The Wugongshan Mesozoic granitoids have higher ISr values (0.70981–0.72885) and lower var epsilonNd(T) (−10.6 to −14.7; an average of −12.6) than those of the early Paleozoic Shanzhuang granodiorite. The Mesozoic granitoids were likely derived from ancient sedimentary rocks by partial melting. The Wugongshan Mesozoic granitoids contain three petrological zones, that is, an Early Cretaceous massive granitic zone in the core (Zone I), a foliated granitic zone (Zone II) and a Triassic granitic gneissic zone in the outer-rim (Zone III). The petrological and geochemical features of massive granitoids (Zone I) are similar to those of foliated granites (Zone II) and of granitic gneisses (Zone III) in this Mesozoic dome. Moreover, geometric and kinematic features within the ductile parts (Units 2 and 3) are also similar to those within the brittle part (Unit 1) of the dome. All these features show that the geologic evolution of the Wugongshan doming is a continuous process lasting from Triassic to Early Cretaceous time. Published 40Ar/39Ar and K–Ar ages in the Wugongshan Mesozoic granitic rocks fall into two major age fields, corresponding to two geodynamic events of intracontinental deformation and magmatic activity. The first tectonothermal event, dated at 226–259 Ma on the granitic gneisses in the outer-rim of dome, can be linked to Indosinian collision between the South China plate and the North China plate during Triassic time. The second event took place during the Early Yanshanian, dated at 180–120 Ma on the granites of the core of dome, and are responsible for final doming of the Wugongshan plutons. This event may be related to a westward subduction of the Paleo-Pacific oceanic plate under the SE-China continent during Late Jurassic–Early Cretaceous time.
Georgiy A Guriev - One of the best experts on this subject based on the ideXlab platform.
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influence of syn sedimentary faults on orogenic structure examples from the neoproterozoic Mesozoic east siberian passive margin
Tectonophysics, 2003Co-Authors: A K Khudoley, Georgiy A GurievAbstract:Abstract The east margin of the Siberian craton is a typical passive margin with a thick succession of sedimentary rocks ranging in age from Mesoproterozoic to Tertiary. Several zones with distinct structural styles are recognized and reflect an eastward-migrating depocenter. Mesozoic orogeny was preceded by several Mesoproterozoic to Paleozoic tectonic events. In the South Verkhoyansk, the most intense pre-Mesozoic event, 1000–950 Ma rifting, affected the margin of the Siberian craton and formed half-graben basins, bounded by listric normal faults. Neoproterozoic compressional structures occurred locally, whereas extensional structures, related to latest Neoproterozoic–early Paleozoic rifting events, have yet to be identified. Devonian rifting is recognized throughout the eastern margin of the Siberian craton and is represented by numerous normal faults and local half-graben basins. Estimated shortening associated with Mesozoic compression shows that the inner parts of ancient rifts are now hidden beneath late Paleozoic–Mesozoic siliciclastics of the Verkhoyansk Complex and that only the outer parts are exposed in frontal ranges of the Verkhoyansk thrust-and-fold belt. Mesoproterozoic to Paleozoic structures had various impacts on the Mesozoic compressional structures. Rifting at 1000–950 Ma formed extensional detachment and normal faults that were reactivated as thrusts characteristic of the Verkhoyansk foreland. Younger Neoproterozoic compressional structures do not display any evidence for Mesozoic reactivation. Several initially east-dipping Late Devonian normal faults were passively rotated during Mesozoic orogenesis and are now recognized as west-dipping thrusts, but without significant reactivation displacement along fault surfaces.
X M Zhou - One of the best experts on this subject based on the ideXlab platform.
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Mesozoic tectonic evolution of the southeast china block new insights from basin analysis
Journal of Asian Earth Sciences, 2009Co-Authors: X M Zhou, Bo Wang, Xixi Zhao, P Deng, Shaoyong Jiang, Jinhai YuAbstract:Abstract In order to better understand the Mesozoic tectonic evolution of Southeast China Block (SECB in short), this paper describes geological features of Mesozoic basins that are widely distributed in the SECB. The analyzed data are derived from a regional geological investigation on various Mesozoic basins and a recently compiled 1:1,500,000 geological map of Mesozoic–Cenozoic basins. Two types of basin are distinguished according to their tectonic settings, namely, the post-orogenic basin (Type I) and the intracontinental extensional basin (Type II); the latter includes the graben and the half-graben or faulted-depression basins. Our studies suggest that the formation of these basins connects with the evolution of geotectonics of the SECB. The post-orogenic basin (Type I) was formed in areas from the piedmont to the intraland during the interval from Late Triassic to Early Jurassic; and the formation of the intracontinental extensional basin (Type II) connects with an intracontinental crustal thinning setting in the Late Mesozoic. The graben basin was generated during the Middle Jurassic and is associated with a bimodal volcanic eruption; and the half-graben or faulted-depression basin, filled mainly by the rhyolite, tuff and sedimentary rocks during Early Cretaceous, is occupied by the Late Cretaceous–Paleogene red-colored terrestrial clastic rocks. We noticed that the modern outcrops of numerous granites and basins occur in a similar level, and the Mesozoic granitic bodies contact with the adjacent basins by large normal faults, suggesting that the modern landforms between granites and basins were yielded by the late crustal movement. The modern basin and range framework was settled down in the Cretaceous. Abundant sedimentary structures are found in the various basins, from that the deposited environments and paleo-currents are concluded; during the Late Triassic–Early Jurassic time, the source areas were situated to the north and northeast sides of the outcrop region. In this paper, we present the study results on one geological and geographical separating unit and two separating fault zones. The Wuyi orogenic belt is a Late Mesozoic paleo-geographically separating unit, the Ganjiang fault zone behaves as the western boundary of Early Cretaceous volcanic rocks, and the Zhenghe–Dapu fault zone separates the SE-China Coastal Late Mesozoic volcanic-sedimentary basins and the Wuyi orogenic belt. Finally, we discuss the geodynamic mechanisms forming various basins, proposing a three-stage model of the Mesozoic sedimentary evolution.
