华南中生代大地构造过程
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摘要
华南大陆以规模宏大的中生代陆内变形和火成岩省为典型特征,其不仅为研究东亚大陆中生代大地构造过程的关键地区,更为了解板块边界的俯冲或碰撞作用如何控制陆内变形及陆内造山带形成的理想地区。为了更好的理解华南中生代构造演化历史,本文选择了位于华南大陆北部的大巴山和中部的沅麻盆地、衡山为主要研究区,展开了详细的构造变形观测和同位素年代学分析。另外,结合白垩纪盆地沉积-变形、岩浆活动和构造应力场演化序列等资料,本文对华南白垩纪大地构造过程进行了重点论述。
华南北部北大巴山韧性剪切带的构造变形和40Ar/39Ar同位素年代学分析证实,北大巴山中生代主要经历了两个阶段的构造变形和演化过程。早期构造变形以沿NW-SE走向剪切带(DSZ-1)的top-to-the-SW逆冲剪切作用为主,晚期构造变形以沿NNW-SSE走向剪切带(DSZ-2)的右行走滑剪切作用为主。韧性剪切带中同变形的黑云母和白云母40Ar/39Ar年代学测试结果证实,这两期构造变形分别形成于中三叠世-早侏罗世(245-189Ma)和中侏罗世-早白垩世(178-143Ma)。早期构造变形与中三叠世-早侏罗世华北和华南板块之间的陆陆碰撞造山作用相关,其导致北大巴山的构造格局初步形成；晚期构造变形与中侏罗世-早白垩世东亚大陆陆内造山作用相关,其造成南秦岭构造带发生向东挤出,并导致南大巴山前陆弧形带的形成。这两期变形事件的识别为理解扬子北缘中生代陆陆碰撞造山和陆内造山作用的构造样式及动力学过程提供了关键证据。另外,北大巴山凤凰山基底隆起8个样品的磷灰石裂变径迹年代学分析和热历史模拟表明,中晚侏罗世陆内挤压造山结束后,凤凰山隆起主要经历了两个阶段的构造隆升历史：早白垩世(135-+5-95-+5Ma)缓慢隆升,晚白垩世(95±5-65-+5Ma)快速隆升。早白垩世缓慢隆升代表了陆内造山结束后的稳定阶段；晚白垩世快速隆升为一次区域性隆升事件,在秦岭、大别和武当等地区均有反映,隆升过程中伴随着强烈的伸展垮塌作用,沿秦岭造山带发育一系列伸展断陷盆地。
华南大陆中部的沅麻盆地夹于古太平洋和特提斯两大构造域的中间位置,其距两侧活动板块边界>800km,是理解华南晚中生代-新生代构造演化过程的关键地区。通过对不同地层单元断层滑动矢量的统计分析,本文建立了沅麻盆地晚中生代-新生代五个阶段的构造变形及古构造应力场演化历史。中晚侏罗世,构造应力场以E-W挤压为主,其导致沅麻盆地东缘前白垩系发生广泛冲断褶皱变形,形成NNE-SSW向褶皱及逆冲推覆构造。这期挤压强烈影响了整个华南大陆,导致壮观的宽约1300km陆内褶皱冲断带的形成。早白垩世初,构造应力场转变为NW-SE(?)申展,其控制着沅麻盆地的初始伸展断陷和沉积物的充填,奠定了沅麻盆地的构造格局。这期伸展引发华南陆壳发生强烈伸展断陷,形成一系列伸展盆地,并诱发了大规模的岩浆侵位和火山作用。早白垩世晚期的NW-SE挤压,导致沅麻盆地结束断陷沉积,并发生构造反转,同时,其诱发大型NNE走向断裂／剪切带左行走滑剪切,并终止了与伸展相关的活动大陆边缘岩浆活动。晚白垩世,古构造应力场转变为N-S伸展,其导致沅麻盆地沿E-W断裂张开并再次发生伸展断陷作用。这期伸展可持续至古近纪早期,并被古近纪晚期的NE-SW挤压所终止。NE-SW挤压导致华南大陆古近系广泛褶皱并发生整体隆升剥蚀,形成古近系和新近系之间区域性角度不整合面。沅麻盆地古构造应力场的交替和演化与华南周缘板块晚中生代-新生代的动力学过程密切相关。中侏罗世E-W挤压和早白垩世NW-SE(?)申展／挤压源于古太平洋板块向亚洲大陆的NW向俯冲作用；晚白垩世-古近纪的N-S伸展和NE-SW挤压,分别与印度板块向亚洲大陆的俯冲作用和二者随后的陆陆碰撞作用有关。
本文在华南中部识别出一条大尺度的低角度拆离断裂,将其命名为衡山主拆离断裂。这条断裂沿NNE-NE走向延伸>150kmm,并横穿江南造山带,其规模与北美科迪勒拉造山带壮观的Whipple主拆离断裂可比。在断裂的南部,沿下盘发育一条约3km宽的低角度韧性剪切带,与衡山复式花岗岩体的西缘相接。笔者对该剪切带展开了详细构造变形和同位素年代学研究,结果表明,在剪切带北部,糜棱面理走向NE-SW,其上的拉伸线理向NW倾伏,运动方向为top-to-the-NW伸展剪切；在剪切带南部,糜棱面理走向NW-SE,其上的拉伸线理向SW倾伏,运动方向为top-to-the-SW伸展剪切。剪切带中糜棱岩的石英c轴组构型式表现为不对称的单环带或Ⅰ型交叉环带,其极密区的分布型式反映了底面和柱面滑移系的共同作用,表明伸展剪切变形温度约为400～550℃。剪切带中同构造钠长岩脉的SHRIMP锆石U-Pb年代学和糜棱岩中白云母40Ar/39Ar年龄表明,衡山低角度伸展剪切变形的持续时间为136～97Ma。5个花岗岩的SHRIMP锆石U-Pb测试结果证实,衡山复式花岗岩体为232-228Ma和150-151Ma两期岩浆侵位形成,其最年轻岩浆的侵位时代比剪切带的伸展剪切变形早15Myr。由此可知,衡山地区缺少与剪切变形同期的花岗质岩体的侵位。另外,衡山主拆离断裂的形成机制不同于经典变质核杂岩中低角度拆离断裂,其为早期低角度逆冲断裂复活并发生负反转变形的产物。因此,从严格意义上讲,衡山应定义为一个伸展穹窿或低角度拆离带,而非变质核杂岩。本次研究不仅证实华南早白垩世大规模地壳伸展作用起始于136Ma,同时为理解大陆伸展过程中上地壳和中地壳的变形样式提供了重要参考。
华南白垩纪构造演化以大规模的伸展断陷盆地形成、岩浆侵位和火山作用及多金属矿化作用为典型特征,这些变形、岩浆与成矿作用在全球中生代构造演化中独具特色,一直为国内外地质学家关注的焦点。由于缺乏对华南大陆白垩纪构造演化过程及动力学机制的全面理解,关于这些地质现象的性质及动力学成因,一直存在争议。本文重点对华南白垩纪盆地沉积-变形、岩浆活动和构造应力场演化序列进行了系统分析和梳理,建立了华南大陆白垩纪六个阶段的构造-岩浆演化过程,并讨论了各个阶段演化的地球动力学机制。早白垩世早期(145-137Ma)挤压作用,导致(1)长江中下游地区俯冲洋壳或地壳加厚熔融形成埃达克质岩,并伴随着Cu-Au等多金属矿床的形成；(2)东南沿海地区地壳加厚重熔,形成片麻状花岗岩和混合花岗岩,其形成机制与古太平洋和伊泽奈崎板块之间的大洋中脊俯冲作用密切相关。早白垩世中期(136-118Ma),古构造应力场转变为NW-SE伸展,其导致一系列伸展断陷盆地的形成,并诱发了大规模的岩浆侵位和火山活动。在长江中下游地区,这期伸展的动力学机制与洋中脊的持续俯冲作用有关；在华夏板块,这期伸展与古太平洋板块俯冲过程中的板片后撤诱发的弧后扩张作用有关。中白垩世NW-SE挤压(117-108Ma)终止了与伸展相关的活动大陆边缘岩浆活动,并引发了断陷盆地的广泛构造反转及NE-SW断裂／剪切带的左行走滑剪切作用,这期挤压可能与西菲律宾微板块和亚洲大陆的碰撞作用相关。中-晚白垩世NW-SE(?)申展(107-87Ma)和随后的WNW-ESE挤压引发了华南白垩纪第二次大规模的地壳伸展和构造反转,这两个阶段间古构造应力场从伸展到挤压的明显变动可能与古太平洋板块俯冲角度的变化有关。晚白垩世末期,随着华南周缘板块动力学过程的重大调整,古构造应力场转变为N-S伸展,其形成可能与新特提斯构造域印度板块向亚洲大陆俯冲过程中诱发的弧后扩张作用有关。
The South China block, featured by rich and complex patterns of Mesozoic intracontinental deformation and large igneous provinces, is one of the most optimal areas in the world to understand not also the Mesozoic geological architecture of East Asia, but also how the subduction or collision occurring in the plate boundaries controls the formation of intracontinental orogeny and deformation. In order to clarify the deformation features and decipher the tectonic evolution of South China during the Mesozoic period, detailed structural and geochronological studies have been conducted in the Dabashan, Yuanma Basin and Hengshan massif. Moreover, an overall review for the Cretaceous tectonics in South China by considering multiple lines of evidence is given to constrain the Cretaceous tectonic evolution, and to aid in directing future research of South China.
Structural and40Ar/39Ar data from the mylonitic rocks of the North Dabashan zone (NDZ) document kinematic and tectonothermal characteristics of the Mesozoic collisional and intra-continental orogenesis in the northern segment of Yangtze Block. The NDZ underwent two deformational phases during the Mesozoic period. The earlier one is characterized by top-to-the-SW thrust ductile shearing along a NW-trending shear zone (DSZ-1), while the later one is featured by dextral strike-slip ductile shearing along another NNW-trending shear zone (DSZ-2). The timing of the two deformation events have been constrained to be245-189Ma and178-143Ma respectively, by using mica40Ar/39Ar geochronology It is proposed that the earlier deformation event was associated with the Middle Triassic-Early Jurassic collision between the North and South China Blocks, which generated the initial framework of the NDZ; and the later one was related to the Middle Jurassic to Early Cretaceous intra-continental orogeny in East Asia, which caused a significant eastward extrusion of the South Qinling and led to the formation of the SW-convex Dabashan foreland orocline. The distinguishing between these two deformation events sheds a new insight into the Mesozoic tectonic evolution of the Qinling orogenic belt. Apatite fission track (AFT) dating and thermal modeling were carried out on eight rock samples collected from the Fenghuangshan massif in the North Dabashan zone. The results show that the uplifting history of Fenghuangshan massif can be divided into two stages during the Cretaceous period:Early Cretaceous slow (135±5～95±5Ma) and Late Cretaceous rapid uplifting (95±5～65±5Ma). The former one represented a period of relative stability after the Late Jurassic intracontinental orogenesis within the Dabashan structural belt; while the latter one was concomitant with post-orogenic extension and collapse of the Dabashan structural belt, during which arrays of coeval rifted basins had been generated along the Qinling orogenic belt.
The Yuanma Basin, situated in central South China with more than800km far away from the active plate boundaries, is a key region in deciphering the Late Mesozoic-Early Cenozoic tectonic evolution of South China. Based on a field analysis of fault-slip data collected from different rock units, we document polyphase tectonic stress fields and address the changes in the orientation of the principal stresses, and finally establish a five-phase stress evolution of the basin during the Late Mesozoic-Early Cenozoic. The earliest one with E-W compression and N-S extension occurred in the Mid-Late Jurassic and resulted in regional folding and west-directed thrusting along the eastern margin of the basin. This deformational event constrains the timing of the significant intracontinental orogeny in South China to be Mid-Late Jurassic. The subsequent NW-SE extensional regime was responsible for the initial opening and sedimentary infill of the basin during the earliest Cretaceous, which occurred coevally with the extensive Early Cretaceous magmatism, volcanism and extensional doming in South China. The tectonic regime then changed, in the late Early Cretaceous, to a compressional one with NW-SE compression and NE-SW extension, causing the inversion of this extensional basin. This compression affected the whole South China, leading to an apparent magmatic quiescence at～108-117Ma and sinistral strike-slip faulting on the NNE-trending faults. The N-S extension prevailed in the Late Cretaceous, and activated the east-trending normal faults that controlled the Late Cretaceous subsidence. This extensional phase seems to have lasted through the Early Paleogene and ended in the Late Paleogene by a compressional regime with NE-SW compression and NW-SE extension, as attested by the stratigraphic unconformity at the base of the Neogene in the Jianghan Basin. The temporary evolution of these tectonic stress fields documented in the Yuanma Basin provides a new insight into the influences of different plate tectonics exerting on the South China Block over the Late Mesozoic to Early Cenozoic time. We infer that the Yuanma basin was influenced, in the Middle Jurassic-Early Cretaceous, by the process of westward subduction of paleo-Pacific plate; and in the Late Cretaceous-Early Paleogene by a combined effect of the subduction along the west pacific margin and in the Tethyan domain; and finally in the Late Paleogene by the far-field effects of India-Asia collision.
A significant low-angle normal fault, namely the Hengshan detachment fault, has been documented in the Jiangnan orogenic belt, which extends more than150km long in NNE orientation and bounds an elongated Early Cretaceous basin in Hunan Province, central South China. Detailed structural and geochronological analyses have been conducted along its southern segment, where a well exposed,～3km thick, flat ductile shear zone develops along the western margin of the Hengshan granitic massif. This zone is featured by shallow-dipping foliations of varied trend from NE to NW, which bear penetrative stretching lineations varying from NW to SW trend. Shear sense criteria indicate top-to-the-NW and top-to-the-SW motions along its northern and southern parts, respectively. Quartz c-axis orientations of mylonitic rocks from the shear zone exhibit asymmetric single or crossed girdle patterns, and the distributions of fabric point maxima suggest a simultaneous operation of basal and prism slips, indicating a deformation temperature ranging from400℃to550癈.℃One zircon U-Pb age of the sheared albitite and three muscovite40Ar/39Ar ages of the mylonitic rocks indicate that the ductile shearing initiated at136Ma and lasted till97Ma. The zircon U-Pb dating results of five granitic samples from the Hengshan granitic pluton yield two phases of crystallization ages of232-228Ma and150-151Ma respectively, indicating two preceding magmatic events prior to the ductile shearing in the lower plate. Our structural and geochronological data allow defining the Hengshan massif as an extensional dome, rather than a metamorphic core complex as previously predicted, due to the lack of syn-tectonic plutonism and the origin of detachment fault associated with the reactivation of inherited thrust. This study provides crucial evidence for understanding how the mid-upper crust deformed during the process of extension, which testifies to a coeval occurrence of non-coaxial deformation of the ductile flow in the middle crust and brittle faulting in the upper crust. It also sheds new insights into the timing of the regional crustal extension in South China, and permits to constrain its onset time to be ca.136Ma.
The Cretaceous tectonics of South China is characterized by widespread extensional basins, voluminous magma intrusion/eruption and associated polymetallic mineralization, all of which are of world-wide interests and have stimulated the attention of geologists for more than half a century. The controversies regarding the nature and origin of these features rise from a lack of comprehensive understanding of the regional tectonic evolution and geodynamics of South China. This paper attempts to make a review by synthesizing existing structural, petrological, geochronological and geochemical data of the Cretaceous basins and magmatism, and to propose a chronology of six-stage tectono-thermal evolutionary history of South China during the Cretaceous. The earliest Cretaceous compression (145-137Ma) led to the formation of adakitic rocks and associated Cu-Au deposits in the Lower Yangtze River Belt and the gneissic granites in the coastal area, formation of them were possibly related to the midocean ridge subduction of the Paleo-Pacific and Izanagi plates. The middle Cretaceous (136-118Ma) was predominated by the NW-SE extensional regime, which led to significant taphrogenesis manifested by large-scale extensional basins and voluminous magma intrusion/eruption, formation of them might have resulted from a combination of ridge subduction and rollback of the subducted oceanic slab of the Paleo-Pacific plate. This extensional stage was followed during the latest Early Cretaceous (117-108Ma) by a NW-SE-oriented compressional one, which led to cessation of the active marginal magmatism and caused tectonic inversion of previous rift basins and sinistral strike-slip faulting along the NE-striking faults. This compression is attributed to the collision between the eastern Asian margin and the West Philippine block. The collision-induced crustal contraction was quickly terminated by a WNW-ESE extensional regime during the Mid-Late Cretaceous (107-86Ma), which led to a new phase of basin subsidence and magmatism particularly along the coastal area of South China. Then a WNW-ESE compressional regime settled down in South China during the Late Cretaceous, which resulted in a second tectonic inversion of the Cretaceous basins. The changes in tectonic regime may be due to the break-off or changing geometries of the subducted oceanic slab beneath South China. Plate kinematics seems to have changed dramatically during the late Cretaceous when a N-S extensional stress regime prevailed over South China, which might result from a far-field effect produced by northward subduction of the Neo-Tethys oceanic plate beneath the southwestern margin of South China.
华南北部北大巴山韧性剪切带的构造变形和40Ar/39Ar同位素年代学分析证实,北大巴山中生代主要经历了两个阶段的构造变形和演化过程。早期构造变形以沿NW-SE走向剪切带(DSZ-1)的top-to-the-SW逆冲剪切作用为主,晚期构造变形以沿NNW-SSE走向剪切带(DSZ-2)的右行走滑剪切作用为主。韧性剪切带中同变形的黑云母和白云母40Ar/39Ar年代学测试结果证实,这两期构造变形分别形成于中三叠世-早侏罗世(245-189Ma)和中侏罗世-早白垩世(178-143Ma)。早期构造变形与中三叠世-早侏罗世华北和华南板块之间的陆陆碰撞造山作用相关,其导致北大巴山的构造格局初步形成；晚期构造变形与中侏罗世-早白垩世东亚大陆陆内造山作用相关,其造成南秦岭构造带发生向东挤出,并导致南大巴山前陆弧形带的形成。这两期变形事件的识别为理解扬子北缘中生代陆陆碰撞造山和陆内造山作用的构造样式及动力学过程提供了关键证据。另外,北大巴山凤凰山基底隆起8个样品的磷灰石裂变径迹年代学分析和热历史模拟表明,中晚侏罗世陆内挤压造山结束后,凤凰山隆起主要经历了两个阶段的构造隆升历史：早白垩世(135-+5-95-+5Ma)缓慢隆升,晚白垩世(95±5-65-+5Ma)快速隆升。早白垩世缓慢隆升代表了陆内造山结束后的稳定阶段；晚白垩世快速隆升为一次区域性隆升事件,在秦岭、大别和武当等地区均有反映,隆升过程中伴随着强烈的伸展垮塌作用,沿秦岭造山带发育一系列伸展断陷盆地。
华南大陆中部的沅麻盆地夹于古太平洋和特提斯两大构造域的中间位置,其距两侧活动板块边界>800km,是理解华南晚中生代-新生代构造演化过程的关键地区。通过对不同地层单元断层滑动矢量的统计分析,本文建立了沅麻盆地晚中生代-新生代五个阶段的构造变形及古构造应力场演化历史。中晚侏罗世,构造应力场以E-W挤压为主,其导致沅麻盆地东缘前白垩系发生广泛冲断褶皱变形,形成NNE-SSW向褶皱及逆冲推覆构造。这期挤压强烈影响了整个华南大陆,导致壮观的宽约1300km陆内褶皱冲断带的形成。早白垩世初,构造应力场转变为NW-SE(?)申展,其控制着沅麻盆地的初始伸展断陷和沉积物的充填,奠定了沅麻盆地的构造格局。这期伸展引发华南陆壳发生强烈伸展断陷,形成一系列伸展盆地,并诱发了大规模的岩浆侵位和火山作用。早白垩世晚期的NW-SE挤压,导致沅麻盆地结束断陷沉积,并发生构造反转,同时,其诱发大型NNE走向断裂／剪切带左行走滑剪切,并终止了与伸展相关的活动大陆边缘岩浆活动。晚白垩世,古构造应力场转变为N-S伸展,其导致沅麻盆地沿E-W断裂张开并再次发生伸展断陷作用。这期伸展可持续至古近纪早期,并被古近纪晚期的NE-SW挤压所终止。NE-SW挤压导致华南大陆古近系广泛褶皱并发生整体隆升剥蚀,形成古近系和新近系之间区域性角度不整合面。沅麻盆地古构造应力场的交替和演化与华南周缘板块晚中生代-新生代的动力学过程密切相关。中侏罗世E-W挤压和早白垩世NW-SE(?)申展／挤压源于古太平洋板块向亚洲大陆的NW向俯冲作用；晚白垩世-古近纪的N-S伸展和NE-SW挤压,分别与印度板块向亚洲大陆的俯冲作用和二者随后的陆陆碰撞作用有关。
本文在华南中部识别出一条大尺度的低角度拆离断裂,将其命名为衡山主拆离断裂。这条断裂沿NNE-NE走向延伸>150kmm,并横穿江南造山带,其规模与北美科迪勒拉造山带壮观的Whipple主拆离断裂可比。在断裂的南部,沿下盘发育一条约3km宽的低角度韧性剪切带,与衡山复式花岗岩体的西缘相接。笔者对该剪切带展开了详细构造变形和同位素年代学研究,结果表明,在剪切带北部,糜棱面理走向NE-SW,其上的拉伸线理向NW倾伏,运动方向为top-to-the-NW伸展剪切；在剪切带南部,糜棱面理走向NW-SE,其上的拉伸线理向SW倾伏,运动方向为top-to-the-SW伸展剪切。剪切带中糜棱岩的石英c轴组构型式表现为不对称的单环带或Ⅰ型交叉环带,其极密区的分布型式反映了底面和柱面滑移系的共同作用,表明伸展剪切变形温度约为400～550℃。剪切带中同构造钠长岩脉的SHRIMP锆石U-Pb年代学和糜棱岩中白云母40Ar/39Ar年龄表明,衡山低角度伸展剪切变形的持续时间为136～97Ma。5个花岗岩的SHRIMP锆石U-Pb测试结果证实,衡山复式花岗岩体为232-228Ma和150-151Ma两期岩浆侵位形成,其最年轻岩浆的侵位时代比剪切带的伸展剪切变形早15Myr。由此可知,衡山地区缺少与剪切变形同期的花岗质岩体的侵位。另外,衡山主拆离断裂的形成机制不同于经典变质核杂岩中低角度拆离断裂,其为早期低角度逆冲断裂复活并发生负反转变形的产物。因此,从严格意义上讲,衡山应定义为一个伸展穹窿或低角度拆离带,而非变质核杂岩。本次研究不仅证实华南早白垩世大规模地壳伸展作用起始于136Ma,同时为理解大陆伸展过程中上地壳和中地壳的变形样式提供了重要参考。
华南白垩纪构造演化以大规模的伸展断陷盆地形成、岩浆侵位和火山作用及多金属矿化作用为典型特征,这些变形、岩浆与成矿作用在全球中生代构造演化中独具特色,一直为国内外地质学家关注的焦点。由于缺乏对华南大陆白垩纪构造演化过程及动力学机制的全面理解,关于这些地质现象的性质及动力学成因,一直存在争议。本文重点对华南白垩纪盆地沉积-变形、岩浆活动和构造应力场演化序列进行了系统分析和梳理,建立了华南大陆白垩纪六个阶段的构造-岩浆演化过程,并讨论了各个阶段演化的地球动力学机制。早白垩世早期(145-137Ma)挤压作用,导致(1)长江中下游地区俯冲洋壳或地壳加厚熔融形成埃达克质岩,并伴随着Cu-Au等多金属矿床的形成；(2)东南沿海地区地壳加厚重熔,形成片麻状花岗岩和混合花岗岩,其形成机制与古太平洋和伊泽奈崎板块之间的大洋中脊俯冲作用密切相关。早白垩世中期(136-118Ma),古构造应力场转变为NW-SE伸展,其导致一系列伸展断陷盆地的形成,并诱发了大规模的岩浆侵位和火山活动。在长江中下游地区,这期伸展的动力学机制与洋中脊的持续俯冲作用有关；在华夏板块,这期伸展与古太平洋板块俯冲过程中的板片后撤诱发的弧后扩张作用有关。中白垩世NW-SE挤压(117-108Ma)终止了与伸展相关的活动大陆边缘岩浆活动,并引发了断陷盆地的广泛构造反转及NE-SW断裂／剪切带的左行走滑剪切作用,这期挤压可能与西菲律宾微板块和亚洲大陆的碰撞作用相关。中-晚白垩世NW-SE(?)申展(107-87Ma)和随后的WNW-ESE挤压引发了华南白垩纪第二次大规模的地壳伸展和构造反转,这两个阶段间古构造应力场从伸展到挤压的明显变动可能与古太平洋板块俯冲角度的变化有关。晚白垩世末期,随着华南周缘板块动力学过程的重大调整,古构造应力场转变为N-S伸展,其形成可能与新特提斯构造域印度板块向亚洲大陆俯冲过程中诱发的弧后扩张作用有关。
The South China block, featured by rich and complex patterns of Mesozoic intracontinental deformation and large igneous provinces, is one of the most optimal areas in the world to understand not also the Mesozoic geological architecture of East Asia, but also how the subduction or collision occurring in the plate boundaries controls the formation of intracontinental orogeny and deformation. In order to clarify the deformation features and decipher the tectonic evolution of South China during the Mesozoic period, detailed structural and geochronological studies have been conducted in the Dabashan, Yuanma Basin and Hengshan massif. Moreover, an overall review for the Cretaceous tectonics in South China by considering multiple lines of evidence is given to constrain the Cretaceous tectonic evolution, and to aid in directing future research of South China.
Structural and40Ar/39Ar data from the mylonitic rocks of the North Dabashan zone (NDZ) document kinematic and tectonothermal characteristics of the Mesozoic collisional and intra-continental orogenesis in the northern segment of Yangtze Block. The NDZ underwent two deformational phases during the Mesozoic period. The earlier one is characterized by top-to-the-SW thrust ductile shearing along a NW-trending shear zone (DSZ-1), while the later one is featured by dextral strike-slip ductile shearing along another NNW-trending shear zone (DSZ-2). The timing of the two deformation events have been constrained to be245-189Ma and178-143Ma respectively, by using mica40Ar/39Ar geochronology It is proposed that the earlier deformation event was associated with the Middle Triassic-Early Jurassic collision between the North and South China Blocks, which generated the initial framework of the NDZ; and the later one was related to the Middle Jurassic to Early Cretaceous intra-continental orogeny in East Asia, which caused a significant eastward extrusion of the South Qinling and led to the formation of the SW-convex Dabashan foreland orocline. The distinguishing between these two deformation events sheds a new insight into the Mesozoic tectonic evolution of the Qinling orogenic belt. Apatite fission track (AFT) dating and thermal modeling were carried out on eight rock samples collected from the Fenghuangshan massif in the North Dabashan zone. The results show that the uplifting history of Fenghuangshan massif can be divided into two stages during the Cretaceous period:Early Cretaceous slow (135±5～95±5Ma) and Late Cretaceous rapid uplifting (95±5～65±5Ma). The former one represented a period of relative stability after the Late Jurassic intracontinental orogenesis within the Dabashan structural belt; while the latter one was concomitant with post-orogenic extension and collapse of the Dabashan structural belt, during which arrays of coeval rifted basins had been generated along the Qinling orogenic belt.
The Yuanma Basin, situated in central South China with more than800km far away from the active plate boundaries, is a key region in deciphering the Late Mesozoic-Early Cenozoic tectonic evolution of South China. Based on a field analysis of fault-slip data collected from different rock units, we document polyphase tectonic stress fields and address the changes in the orientation of the principal stresses, and finally establish a five-phase stress evolution of the basin during the Late Mesozoic-Early Cenozoic. The earliest one with E-W compression and N-S extension occurred in the Mid-Late Jurassic and resulted in regional folding and west-directed thrusting along the eastern margin of the basin. This deformational event constrains the timing of the significant intracontinental orogeny in South China to be Mid-Late Jurassic. The subsequent NW-SE extensional regime was responsible for the initial opening and sedimentary infill of the basin during the earliest Cretaceous, which occurred coevally with the extensive Early Cretaceous magmatism, volcanism and extensional doming in South China. The tectonic regime then changed, in the late Early Cretaceous, to a compressional one with NW-SE compression and NE-SW extension, causing the inversion of this extensional basin. This compression affected the whole South China, leading to an apparent magmatic quiescence at～108-117Ma and sinistral strike-slip faulting on the NNE-trending faults. The N-S extension prevailed in the Late Cretaceous, and activated the east-trending normal faults that controlled the Late Cretaceous subsidence. This extensional phase seems to have lasted through the Early Paleogene and ended in the Late Paleogene by a compressional regime with NE-SW compression and NW-SE extension, as attested by the stratigraphic unconformity at the base of the Neogene in the Jianghan Basin. The temporary evolution of these tectonic stress fields documented in the Yuanma Basin provides a new insight into the influences of different plate tectonics exerting on the South China Block over the Late Mesozoic to Early Cenozoic time. We infer that the Yuanma basin was influenced, in the Middle Jurassic-Early Cretaceous, by the process of westward subduction of paleo-Pacific plate; and in the Late Cretaceous-Early Paleogene by a combined effect of the subduction along the west pacific margin and in the Tethyan domain; and finally in the Late Paleogene by the far-field effects of India-Asia collision.
A significant low-angle normal fault, namely the Hengshan detachment fault, has been documented in the Jiangnan orogenic belt, which extends more than150km long in NNE orientation and bounds an elongated Early Cretaceous basin in Hunan Province, central South China. Detailed structural and geochronological analyses have been conducted along its southern segment, where a well exposed,～3km thick, flat ductile shear zone develops along the western margin of the Hengshan granitic massif. This zone is featured by shallow-dipping foliations of varied trend from NE to NW, which bear penetrative stretching lineations varying from NW to SW trend. Shear sense criteria indicate top-to-the-NW and top-to-the-SW motions along its northern and southern parts, respectively. Quartz c-axis orientations of mylonitic rocks from the shear zone exhibit asymmetric single or crossed girdle patterns, and the distributions of fabric point maxima suggest a simultaneous operation of basal and prism slips, indicating a deformation temperature ranging from400℃to550癈.℃One zircon U-Pb age of the sheared albitite and three muscovite40Ar/39Ar ages of the mylonitic rocks indicate that the ductile shearing initiated at136Ma and lasted till97Ma. The zircon U-Pb dating results of five granitic samples from the Hengshan granitic pluton yield two phases of crystallization ages of232-228Ma and150-151Ma respectively, indicating two preceding magmatic events prior to the ductile shearing in the lower plate. Our structural and geochronological data allow defining the Hengshan massif as an extensional dome, rather than a metamorphic core complex as previously predicted, due to the lack of syn-tectonic plutonism and the origin of detachment fault associated with the reactivation of inherited thrust. This study provides crucial evidence for understanding how the mid-upper crust deformed during the process of extension, which testifies to a coeval occurrence of non-coaxial deformation of the ductile flow in the middle crust and brittle faulting in the upper crust. It also sheds new insights into the timing of the regional crustal extension in South China, and permits to constrain its onset time to be ca.136Ma.
The Cretaceous tectonics of South China is characterized by widespread extensional basins, voluminous magma intrusion/eruption and associated polymetallic mineralization, all of which are of world-wide interests and have stimulated the attention of geologists for more than half a century. The controversies regarding the nature and origin of these features rise from a lack of comprehensive understanding of the regional tectonic evolution and geodynamics of South China. This paper attempts to make a review by synthesizing existing structural, petrological, geochronological and geochemical data of the Cretaceous basins and magmatism, and to propose a chronology of six-stage tectono-thermal evolutionary history of South China during the Cretaceous. The earliest Cretaceous compression (145-137Ma) led to the formation of adakitic rocks and associated Cu-Au deposits in the Lower Yangtze River Belt and the gneissic granites in the coastal area, formation of them were possibly related to the midocean ridge subduction of the Paleo-Pacific and Izanagi plates. The middle Cretaceous (136-118Ma) was predominated by the NW-SE extensional regime, which led to significant taphrogenesis manifested by large-scale extensional basins and voluminous magma intrusion/eruption, formation of them might have resulted from a combination of ridge subduction and rollback of the subducted oceanic slab of the Paleo-Pacific plate. This extensional stage was followed during the latest Early Cretaceous (117-108Ma) by a NW-SE-oriented compressional one, which led to cessation of the active marginal magmatism and caused tectonic inversion of previous rift basins and sinistral strike-slip faulting along the NE-striking faults. This compression is attributed to the collision between the eastern Asian margin and the West Philippine block. The collision-induced crustal contraction was quickly terminated by a WNW-ESE extensional regime during the Mid-Late Cretaceous (107-86Ma), which led to a new phase of basin subsidence and magmatism particularly along the coastal area of South China. Then a WNW-ESE compressional regime settled down in South China during the Late Cretaceous, which resulted in a second tectonic inversion of the Cretaceous basins. The changes in tectonic regime may be due to the break-off or changing geometries of the subducted oceanic slab beneath South China. Plate kinematics seems to have changed dramatically during the late Cretaceous when a N-S extensional stress regime prevailed over South China, which might result from a far-field effect produced by northward subduction of the Neo-Tethys oceanic plate beneath the southwestern margin of South China.
引文
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