The SHRIMP U-Pb zircon dating result of the Tongshi magmatic complex in western Shandong is presented in this paper. The Tongshi magmatic complex comprises fine-grained porphyritic diorite and syenitic porphyry. Eight...The SHRIMP U-Pb zircon dating result of the Tongshi magmatic complex in western Shandong is presented in this paper. The Tongshi magmatic complex comprises fine-grained porphyritic diorite and syenitic porphyry. Eighteen analyses for fine-grained porphyritic diorite gave two concordia ages, in which ten analyses constitute the young age group, giving ^206Pb/^238U ages ranging from 167.9 Ma to 183 Ma with a weighted mean age of 175.7±3.8 Ma, and the other eight yielded ^207Pb/^206Pb ages of 2502 Ma to 2554 Ma with a weighted mean 2518±11 Ma. Two analyses for syenitic porphyry gave ages of 2485 Ma and 2512 Ma, respectively. The age of 175.7±3.8 Ma indicates that the crystallization of the Tongshi magmatic complex occurred in the Middle Jurassic, whereas that of 2518±11 Ma is interpreted as the age of inherited magmatic zircons in the Neoarchean Wutai period.展开更多
Previous studies on ophiolite and granite revealed that a paleo\|ocean which was referred to as “Proto\|Tethys" developed in north part of western Kunlun in Pt 3～Pz 1.The geotectonic unit in Kuda, western Kunlu...Previous studies on ophiolite and granite revealed that a paleo\|ocean which was referred to as “Proto\|Tethys" developed in north part of western Kunlun in Pt 3～Pz 1.The geotectonic unit in Kuda, western Kunlun is composed of early Paleozoic accretionary complexes and the metamorphic equivalents due to subduction of Proto\|Tethys: Along the Xinzang highway (from Yecheng, Xinjiang to Shiquanhe, Tibet), about 30km north of Kuda, a schistose granodiorite intrudes a thick unit of deformed mafic rocks; Non to weakly metamorphosed early Paleozoic fore\|arc turbidite exposed in Yixiekegou; A set of metamorphic rocks about 20km wide in Kuda which was thought of the Precambrian basement is a large\|scale ductile shear zone determined by detailed field observation and laboratory research; About 10km north of Kuda, there is an undeformed potassic granite batholith intrudes the shear zone.The shear zone mainly consists of parametamorphic rocks and orthometamorphte rocks. Moreover, it contains various kinds of oceanic materials of different origins including fragments of seamounts, oceanic reef limestone and dismembered ophiolite suite, such as dunite, peridotite, gabbro and anorthisite with high number up to 91. The dismembered ophiolite suite may probably represents a remnant oceanic crust that related to the breakup of Rodinia. The parametamorphite rocks is composed of mica\|schist, quartzite and gamete\|mica schist,etc., of which protoliths are sedimentary rocks such as mudstone, sandstone, siliciclastic rocks and impure carbonates that most likely accumulated along the passive continental margin of pelagic sedimentary materials. The orthometamorphic rocks is composed of granitic gneiss and amphibolite,etc. The protoliths of amphibolite is oceanic island basalt of MORB basalt that was accretioned in accretionary complex. The accretionary wedge complex suffers intense ductile strain and metamorphism due to the subduction of Proto\|Tethys with the metamorphic grade reaching the greenschist facies to amphibolite facies. The 40 Ar/ 39 Ar age 451Ma of metamorphic homoblende in amphibolite is interpreted to closely date attainment of maximum metamorphic conditions representing the age of initial subduction at the latest, while the 40 Ar/ 39 Ar age 425Ma of biotite is interpreted as dating the post metamorphic cooling through temperatures required for intracrystalline retention of argon representing the cease of subduction. These data provide significant information on the timing of accretion and the age of the subducted Proto\|Tethys. The whole rock Sm\|Nd isochronal age of amphibolite is problematic 737Ma that maybe represent the rifting age of the Rodinia.展开更多
Many Propositions are made about the mechanism of emplacement of volcanoclastic material in the Bombay volcanic complex. The present paper deals exclusively with the physical features of the deposits laid by a complex...Many Propositions are made about the mechanism of emplacement of volcanoclastic material in the Bombay volcanic complex. The present paper deals exclusively with the physical features of the deposits laid by a complex tectono-magmatic process by making detailed inventory of the different kind of volcanic ejecta exposed in the Bomay Volcanic Complex (BVC), and an attempt has been made to classify the deposits genetically. A subsidenace which was hinted at earlier, may be a possible cauldron in BVC has been proposed, which might be responsible for producing such a varied and complex lithology.展开更多
There is a belt of metamorphic core complexes in the western margin of the Yangtze craton . The geological setting of the belt is similar to that of the Cordilleran metamorphic core complexes . A typical one in this b...There is a belt of metamorphic core complexes in the western margin of the Yangtze craton . The geological setting of the belt is similar to that of the Cordilleran metamorphic core complexes . A typical one in this belt is the Jianglang metamorphic core complex , which has a configuration consisting of three layers : a core complex consisting of Mesoproterozoic schist sequence . a ductile middle slab consisting of Paleozoic meta- sedimentary -basalt characterized by the development of ' folding layer' and an upper cover consisting of Xikang Group which has suffered both buckling and flattening . A detachment fault developed along the contact boundary between the cover and basement causes the omission of Upper Sinian and Cambrian at the base of cover . A lot of normal ductile shear zones developed in the cover causes the thinning of it . All the features show that the early extension results in the thinning of crust , but the formation of the dome and exposure of basement rocks may be the results of superimposing of the E-W directed contraction and the following southward thrusting during Indosinian to Yanshanian orogeny . Syntectonic plutonism and pervasive thermo - metamor-phism in the cover suggest that the thermal uplift also causes the uplift of the MCC .展开更多
Many of the sedimentary basins in western China were formed through the superposition and compounding of at least two previously developed sedimentary basins and in general they can be termed as complex superimposed b...Many of the sedimentary basins in western China were formed through the superposition and compounding of at least two previously developed sedimentary basins and in general they can be termed as complex superimposed basins. The distinct differences between these basins and monotype basins are their discontinuous stratigraphic sedimentation, stratigraphic structure and stratigraphic stress-strain action over geological history. Based on the correlation of chronological age on structural sections, superimposed basins can be divided into five types in this study： （1） continuous sedimentation type superimposed basins, （2） middle and late stratigraphic superimposed basins, （3） early and late stratigraphic superimposed basins, （4） early and middle stratigraphic superimposed basins, and （5） long-term exposed superimposed basins. Multiple source-reservoir-caprock assemblages have developed in such basins. In addition, multi-stage hydrocarbon generation and expulsion, multiple sources, polycyclic hydrocarbon accumulation and multiple-type hydrocarbon reservoirs adjustment, reformation and destruction have occurred in these basins. The complex reservoirs that have been discovered widely in the superimposed basins to date have remarkably different geologic features from primary reservoirs, and the root causes of this are folding, denudation and the fracture effect caused by multiphase tectonic events in the superimposed basins as well as associated seepage, diffusion, spilling, oxidation, degradation and cracking. Based on their genesis characteristics, complex reservoirs are divided into five categories： （1） primary reservoirs, （2） trap adjustment type reservoirs, （3） component variant reservoirs, （4） phase conversion type reservoirs and （5） scale-reformed reservoirs.展开更多
There is a general consensus that most ophiolites formed above subduction zones(Pearce,2003),particularly during forearc extension at subduction initiation(Shervais,2001;Stern,2004;Whattam and Stern,2011).'Supra-S...There is a general consensus that most ophiolites formed above subduction zones(Pearce,2003),particularly during forearc extension at subduction initiation(Shervais,2001;Stern,2004;Whattam and Stern,2011).'Supra-Subduction zone'(SSZ)ophiolites such as the well-studied Tethyan ophiolites,generally display a characteristic sequential evolution from mid-oceanic ridge basalts(MORBs)to island arc tholeiities(IATs)or bonites(BONs)(Pearce,2003;Dilek and Furnes,2009,2011),which were generated in sequence from the decompression melting of asthenospheric mantle and partial melting of subduction-metasomatized depleted mantle(Stern and Bloomer,1992;Dilek and Furnes,2009;Whattam and Stern,2011).However,ophiolites with MORB and/or oceanic-island basalt(OIB)affinities are rare,and their origin and tectonic nature are poorly understood(Boedo et al.,2013;Saccani et al.,2013).It is interesting that the composition of these ophiolites from the central Tibetan Plateau(CTP)is dominated by MORBs and minor OIBs and a distinct lack of IATs and BONs,which is inconsistent with most ophiolites worldwide(Robinson and Zhou,2008;Zhang et al.,2008).But the generation and tectonic nature of these ophiolites are still controversial.*In this study,we present new geochronological,mineralogical and Sr-Nd isotopic data for the Chayong and Xiewu mafic complexes in the western Garzê-Litang suture zone(GLS),a typical Paleo-Tethyan suture crossing the CTP(Fig.1).The Triassic ophiolite in the western GLS has been described by Li et al.(2009),who foundthat it mainly consists of gabbros,diabases,pillow basalts and a few metamorphic peridotites.The ophiolite has been tectonically dismembered and crops out in Triassic clastic rocks and limestones as tectonic blocks.The Chayong and Xiewu mafic complexes are generally regarded as important fragments of the Triassic ophiolites(e.g.,Jin,2006;Li et al.,2009).Zircon LA-ICP-MS U-Pb ages of234±3 Ma and 236±2 Ma can be interpreted as formation times of the Chayong and Xiewu mafic complexes,respectively.The basalts and gabbros of the Chayong complexexhibitenrichedMORB(E-MORB)compositional affinities except for a weak depletion of Nb,Ta and Ti relative to the primitive mantle,whereas the basalts and gabbros of the Xiewu complex display distinct E-MORB and OIB affinities.The geochemical features suggest a probable fractionation of olivine±clinopyroxene±plagioclase as well as insignificant crustal contamination.The geochemical and Sr-Nd isotopic data reveal that the Chayong mafic rocks may have been derived from depleted MORB-type mantle metasomatized by crustal components and Xiewu mafic rocks from enriched lithosphericmantlemetasomatizedbyOIB-like components.The ratios of Zn/Fet,La/Yb and Sm/Yb indicate that these mafic melts were produced by the partial melting of garnet+minor spinel-bearing peridotite or spinel±minor garnet-bearing peridotite.We propose thatback-arcbasinspreadingassociated with OIB/seamount recycling had occurred in the western GLS at least since the Middle Triassic times,and the decompression melting of the depleted MORB-type asthenospheremantleandpartialmeltingof sub-continental lithosphere were metasomatized by plume-related melts,such as OIBs,which led to the generation of the Chayong and Xiewu mafic melts.展开更多
目的观察慢性低氧时大鼠线粒体呼吸链复合体Ⅰ、Ⅱ、Ⅲ、Ⅴ蛋白表达变化并讨论其病理生理学意义。方法成年雄性Wistar大鼠随机分为慢性低氧(4500m,30d)组和对照组,取双侧腓肠肌,分离线粒体,用Clark氧电极法检测线粒体Ⅲ态呼吸(state3,S...目的观察慢性低氧时大鼠线粒体呼吸链复合体Ⅰ、Ⅱ、Ⅲ、Ⅴ蛋白表达变化并讨论其病理生理学意义。方法成年雄性Wistar大鼠随机分为慢性低氧(4500m,30d)组和对照组,取双侧腓肠肌,分离线粒体,用Clark氧电极法检测线粒体Ⅲ态呼吸(state3,ST3)、Ⅳ态呼吸(state4,ST4)和呼吸控制率(respiratory control ratio,RCR),用Western blot检测线粒体呼吸链复合体Ⅰ、Ⅱ、Ⅲ、Ⅴ蛋白的表达。结果慢性低氧组大鼠腓肠肌线粒体ST3和RCR显著低于对照组(P<0.05)。慢性低氧组大鼠腓肠肌线粒体复合体Ⅰ30×103亚基、复合体Ⅱ70×103亚基、复合体Ⅴα亚基蛋白表达量显著低对照组(P<0.05)。2组线粒体ST4和复合体Ⅲ核心亚基2蛋白表达无显著性差异(P>0.05)。结论低氧可调节大鼠骨骼机线粒体复合体蛋白非协同性表达,导致线粒体氧化磷酸化功能下降。展开更多
基金This study was supported by the Major State Basic Rsearch Program of China(grant G1999043211)National Natural Science Foundation of China(grant 40272088).
文摘The SHRIMP U-Pb zircon dating result of the Tongshi magmatic complex in western Shandong is presented in this paper. The Tongshi magmatic complex comprises fine-grained porphyritic diorite and syenitic porphyry. Eighteen analyses for fine-grained porphyritic diorite gave two concordia ages, in which ten analyses constitute the young age group, giving ^206Pb/^238U ages ranging from 167.9 Ma to 183 Ma with a weighted mean age of 175.7±3.8 Ma, and the other eight yielded ^207Pb/^206Pb ages of 2502 Ma to 2554 Ma with a weighted mean 2518±11 Ma. Two analyses for syenitic porphyry gave ages of 2485 Ma and 2512 Ma, respectively. The age of 175.7±3.8 Ma indicates that the crystallization of the Tongshi magmatic complex occurred in the Middle Jurassic, whereas that of 2518±11 Ma is interpreted as the age of inherited magmatic zircons in the Neoarchean Wutai period.
文摘Previous studies on ophiolite and granite revealed that a paleo\|ocean which was referred to as “Proto\|Tethys" developed in north part of western Kunlun in Pt 3～Pz 1.The geotectonic unit in Kuda, western Kunlun is composed of early Paleozoic accretionary complexes and the metamorphic equivalents due to subduction of Proto\|Tethys: Along the Xinzang highway (from Yecheng, Xinjiang to Shiquanhe, Tibet), about 30km north of Kuda, a schistose granodiorite intrudes a thick unit of deformed mafic rocks; Non to weakly metamorphosed early Paleozoic fore\|arc turbidite exposed in Yixiekegou; A set of metamorphic rocks about 20km wide in Kuda which was thought of the Precambrian basement is a large\|scale ductile shear zone determined by detailed field observation and laboratory research; About 10km north of Kuda, there is an undeformed potassic granite batholith intrudes the shear zone.The shear zone mainly consists of parametamorphic rocks and orthometamorphte rocks. Moreover, it contains various kinds of oceanic materials of different origins including fragments of seamounts, oceanic reef limestone and dismembered ophiolite suite, such as dunite, peridotite, gabbro and anorthisite with high number up to 91. The dismembered ophiolite suite may probably represents a remnant oceanic crust that related to the breakup of Rodinia. The parametamorphite rocks is composed of mica\|schist, quartzite and gamete\|mica schist,etc., of which protoliths are sedimentary rocks such as mudstone, sandstone, siliciclastic rocks and impure carbonates that most likely accumulated along the passive continental margin of pelagic sedimentary materials. The orthometamorphic rocks is composed of granitic gneiss and amphibolite,etc. The protoliths of amphibolite is oceanic island basalt of MORB basalt that was accretioned in accretionary complex. The accretionary wedge complex suffers intense ductile strain and metamorphism due to the subduction of Proto\|Tethys with the metamorphic grade reaching the greenschist facies to amphibolite facies. The 40 Ar/ 39 Ar age 451Ma of metamorphic homoblende in amphibolite is interpreted to closely date attainment of maximum metamorphic conditions representing the age of initial subduction at the latest, while the 40 Ar/ 39 Ar age 425Ma of biotite is interpreted as dating the post metamorphic cooling through temperatures required for intracrystalline retention of argon representing the cease of subduction. These data provide significant information on the timing of accretion and the age of the subducted Proto\|Tethys. The whole rock Sm\|Nd isochronal age of amphibolite is problematic 737Ma that maybe represent the rifting age of the Rodinia.
文摘Many Propositions are made about the mechanism of emplacement of volcanoclastic material in the Bombay volcanic complex. The present paper deals exclusively with the physical features of the deposits laid by a complex tectono-magmatic process by making detailed inventory of the different kind of volcanic ejecta exposed in the Bomay Volcanic Complex (BVC), and an attempt has been made to classify the deposits genetically. A subsidenace which was hinted at earlier, may be a possible cauldron in BVC has been proposed, which might be responsible for producing such a varied and complex lithology.
基金The study is supported by the key project of science and technology of the Ministry of Geology and Mineral Resources (NO .85-01-005-1 )
文摘There is a belt of metamorphic core complexes in the western margin of the Yangtze craton . The geological setting of the belt is similar to that of the Cordilleran metamorphic core complexes . A typical one in this belt is the Jianglang metamorphic core complex , which has a configuration consisting of three layers : a core complex consisting of Mesoproterozoic schist sequence . a ductile middle slab consisting of Paleozoic meta- sedimentary -basalt characterized by the development of ' folding layer' and an upper cover consisting of Xikang Group which has suffered both buckling and flattening . A detachment fault developed along the contact boundary between the cover and basement causes the omission of Upper Sinian and Cambrian at the base of cover . A lot of normal ductile shear zones developed in the cover causes the thinning of it . All the features show that the early extension results in the thinning of crust , but the formation of the dome and exposure of basement rocks may be the results of superimposing of the E-W directed contraction and the following southward thrusting during Indosinian to Yanshanian orogeny . Syntectonic plutonism and pervasive thermo - metamor-phism in the cover suggest that the thermal uplift also causes the uplift of the MCC .
基金the National Key Fundamental Research Plan "973" Project(2006CB202308) for funds for this paper
文摘Many of the sedimentary basins in western China were formed through the superposition and compounding of at least two previously developed sedimentary basins and in general they can be termed as complex superimposed basins. The distinct differences between these basins and monotype basins are their discontinuous stratigraphic sedimentation, stratigraphic structure and stratigraphic stress-strain action over geological history. Based on the correlation of chronological age on structural sections, superimposed basins can be divided into five types in this study： （1） continuous sedimentation type superimposed basins, （2） middle and late stratigraphic superimposed basins, （3） early and late stratigraphic superimposed basins, （4） early and middle stratigraphic superimposed basins, and （5） long-term exposed superimposed basins. Multiple source-reservoir-caprock assemblages have developed in such basins. In addition, multi-stage hydrocarbon generation and expulsion, multiple sources, polycyclic hydrocarbon accumulation and multiple-type hydrocarbon reservoirs adjustment, reformation and destruction have occurred in these basins. The complex reservoirs that have been discovered widely in the superimposed basins to date have remarkably different geologic features from primary reservoirs, and the root causes of this are folding, denudation and the fracture effect caused by multiphase tectonic events in the superimposed basins as well as associated seepage, diffusion, spilling, oxidation, degradation and cracking. Based on their genesis characteristics, complex reservoirs are divided into five categories： （1） primary reservoirs, （2） trap adjustment type reservoirs, （3） component variant reservoirs, （4） phase conversion type reservoirs and （5） scale-reformed reservoirs.
基金financially supported by the National Nature Science Foundation of China (Grant 41272079)
文摘There is a general consensus that most ophiolites formed above subduction zones(Pearce,2003),particularly during forearc extension at subduction initiation(Shervais,2001;Stern,2004;Whattam and Stern,2011).'Supra-Subduction zone'(SSZ)ophiolites such as the well-studied Tethyan ophiolites,generally display a characteristic sequential evolution from mid-oceanic ridge basalts(MORBs)to island arc tholeiities(IATs)or bonites(BONs)(Pearce,2003;Dilek and Furnes,2009,2011),which were generated in sequence from the decompression melting of asthenospheric mantle and partial melting of subduction-metasomatized depleted mantle(Stern and Bloomer,1992;Dilek and Furnes,2009;Whattam and Stern,2011).However,ophiolites with MORB and/or oceanic-island basalt(OIB)affinities are rare,and their origin and tectonic nature are poorly understood(Boedo et al.,2013;Saccani et al.,2013).It is interesting that the composition of these ophiolites from the central Tibetan Plateau(CTP)is dominated by MORBs and minor OIBs and a distinct lack of IATs and BONs,which is inconsistent with most ophiolites worldwide(Robinson and Zhou,2008;Zhang et al.,2008).But the generation and tectonic nature of these ophiolites are still controversial.*In this study,we present new geochronological,mineralogical and Sr-Nd isotopic data for the Chayong and Xiewu mafic complexes in the western Garzê-Litang suture zone(GLS),a typical Paleo-Tethyan suture crossing the CTP(Fig.1).The Triassic ophiolite in the western GLS has been described by Li et al.(2009),who foundthat it mainly consists of gabbros,diabases,pillow basalts and a few metamorphic peridotites.The ophiolite has been tectonically dismembered and crops out in Triassic clastic rocks and limestones as tectonic blocks.The Chayong and Xiewu mafic complexes are generally regarded as important fragments of the Triassic ophiolites(e.g.,Jin,2006;Li et al.,2009).Zircon LA-ICP-MS U-Pb ages of234±3 Ma and 236±2 Ma can be interpreted as formation times of the Chayong and Xiewu mafic complexes,respectively.The basalts and gabbros of the Chayong complexexhibitenrichedMORB(E-MORB)compositional affinities except for a weak depletion of Nb,Ta and Ti relative to the primitive mantle,whereas the basalts and gabbros of the Xiewu complex display distinct E-MORB and OIB affinities.The geochemical features suggest a probable fractionation of olivine±clinopyroxene±plagioclase as well as insignificant crustal contamination.The geochemical and Sr-Nd isotopic data reveal that the Chayong mafic rocks may have been derived from depleted MORB-type mantle metasomatized by crustal components and Xiewu mafic rocks from enriched lithosphericmantlemetasomatizedbyOIB-like components.The ratios of Zn/Fet,La/Yb and Sm/Yb indicate that these mafic melts were produced by the partial melting of garnet+minor spinel-bearing peridotite or spinel±minor garnet-bearing peridotite.We propose thatback-arcbasinspreadingassociated with OIB/seamount recycling had occurred in the western GLS at least since the Middle Triassic times,and the decompression melting of the depleted MORB-type asthenospheremantleandpartialmeltingof sub-continental lithosphere were metasomatized by plume-related melts,such as OIBs,which led to the generation of the Chayong and Xiewu mafic melts.
文摘目的观察慢性低氧时大鼠线粒体呼吸链复合体Ⅰ、Ⅱ、Ⅲ、Ⅴ蛋白表达变化并讨论其病理生理学意义。方法成年雄性Wistar大鼠随机分为慢性低氧(4500m,30d)组和对照组,取双侧腓肠肌,分离线粒体,用Clark氧电极法检测线粒体Ⅲ态呼吸(state3,ST3)、Ⅳ态呼吸(state4,ST4)和呼吸控制率(respiratory control ratio,RCR),用Western blot检测线粒体呼吸链复合体Ⅰ、Ⅱ、Ⅲ、Ⅴ蛋白的表达。结果慢性低氧组大鼠腓肠肌线粒体ST3和RCR显著低于对照组(P<0.05)。慢性低氧组大鼠腓肠肌线粒体复合体Ⅰ30×103亚基、复合体Ⅱ70×103亚基、复合体Ⅴα亚基蛋白表达量显著低对照组(P<0.05)。2组线粒体ST4和复合体Ⅲ核心亚基2蛋白表达无显著性差异(P>0.05)。结论低氧可调节大鼠骨骼机线粒体复合体蛋白非协同性表达,导致线粒体氧化磷酸化功能下降。
