Cryogenian ophiolite tectonics and metallogeny of the Central Eastern Desert of Egypt

The Central Eastern Desert (CED) is characterized by the widespread distribution of Neoproterozoic intra-oceanic island arc ophiolitic assemblages. The ophiolitic units have both back-arc and forearc geochemical signatures. The forearc ophiolitic units lie to the west of the back-arc related ones, indicating formation of an intra-oceanic island arc system above an east-dipping subducted slab (present coordinates). Following final accretion of the Neoproterozoic island arc into the western Saharan Metacraton, cordilleran margin magmatism started above a new W-dipping subduction zone due to a plate polarity reversal. We identify two belts in the CED representing ancient arc–forearc and arc–back-arc assemblages. The western arc–forearc belt is delineated by major serpentinite bodies running ～NNW–SSE, marking a suture zone. Ophiolitic units in the back-arc belt to the east show an increase in the subduction geochemical signature from north to south, culminating in the occurrence of bimodal volcanic rocks farther south. This progression in subduction magmatism resulted from diachronous opening of a back-arc basin from north to south, with a bimodal volcanic arc evolving farther to the south. The intra-oceanic island arc units in the CED include coeval Algoma-type banded iron formations (BIFs) and volcanogenic massive sulphide (VMS) deposits. Formation of the BIFs was related to opening of an ocean basin to the north, whereas development of the VMS was related to rifting of the island arc in the south. Gold occurs as vein-type mineral deposits, concentrated along the NNW–SSE arc–forearc belt. The formation of these vein-type gold ore bodies was controlled by the circulation of hydrothermal fluids through serpentinites that resulted in Au mobilization, as constrained by the close spatial association of auriferous quartz veins with serpentinites along the western arc–forearc belt.     

西藏西南部达巴-休古嘎布蛇绿岩带的形成与演化

:该蛇绿岩带的岩体由地幔橄榄岩组成,主要岩石类型是方辉橄榄岩和纯橄榄岩,缺少典型蛇绿岩剖面中的洋壳单元.微量元素和稀土元素特征显示蛇绿岩形成于类似洋中脊的构造环境.笔者提出该区蛇绿岩来源于印度大陆北缘洋盆的洋壳碎片,这个陆缘洋盆与新特提斯洋主体的形成和演化准同步.洋盆的演化模式是:早三叠世,随着印度(冈瓦纳)大陆向南漂移,其北部边缘因引张裂解产生裂谷,于晚三叠世向东开口与新特提斯洋主体连通,洋盆初具洋壳性质,北侧形成阿依拉-仲巴微陆块.侏罗-白垩纪为洋盆洋壳演化期,处于类似洋中脊的构造环境.晚白垩世末洋盆开始闭合.在新特提斯洋板块向北俯冲消减过程中,阿依拉-仲巴微陆块、陆缘洋盆和印度大陆一起随着向北漂移,在印度大陆向北挤压作用下洋盆逐渐收缩以致最终闭合.     

The Rhenohercynian passive margin of SW England: Development,inversion and extensional reactivation

The SW England Rhenohercynian passive margin initiated with rift-related non-marine sedimentation and bimodal magmatism (Late Lockhovian). Continued lithospheric extension resulted in the exhumation of mantle peridotites and limited seafloor spreading (Emsian-Eifelian). Variscan convergence commenced during the Late Eifelian and was coeval with rifting further north. Collision was marked by the Early Carboniferous emergence of deep marine sedimentary/volcanic rocks from the distal continental margin, oceanic lithosphere, pre-rift basement and upper plate gneisses (correlated with the Mid-German Crystalline High of the Saxothuringian Zone). Progressive inversion of the passive margin was strongly influenced by rift basin geometry. Convergence ceased in the Late Carboniferous and was replaced by an extensional regime that reactivated basin controlling/thrust faults and reorientated earlier fabrics (Start-Perranporth Zone). The resultant exhumation of the lower plate was accompanied by emplacement of the Early Permian SW England granites and was contemporaneous with upper plate sedimentary basin formation above the reactivated Rhenohercynian suture. The Rhenohercynian passive margin probably developed in a marginal basin north of the Rheic Ocean or, possibly, a successor basin following its closure. The Lizard ophiolite is unlikely to represent Rheic Ocean floor or associated forearc (SSZ) crust. The Rheic and Rhenohercynian sutures may be coincident or the Rheic suture may be located further south in the Léon Domain.     

CENOZOIC TECTONIC EVOLUTION AND GEODYNAMICS OF KEKEXILI BASIN IN NORTHERN QINGHAI—XIZANG PLATEAU

CENOZOIC TECTONIC EVOLUTION AND GEODYNAMICS OF KEKEXILI BASIN IN NORTHERN QINGHAI—XIZANG PLATEAU     

渤海湾盆地晚中生代以来伸展模式及动力学机制

通过分析盆地区大陆伸展模型参数、火成岩地球化学特征时空演化、岩石圈分层伸展几何学和运动学、应力场-变形场的匹配和演化,文章对渤海湾盆地晚中生代以来伸展断陷的动力学过程进行了系统讨论。晚中生代,盆地北、西部以变质核杂岩模式伸展,南、东部以宽裂陷模式伸展;在岩石圈伸展过程中,地壳变形方式为简单剪切,岩石圈地幔变形方式为纯剪切;盆地处于洋壳俯冲背景下弧后伸展区,盆地及西、北部隆起区岩石圈地幔为EM1型,而南、东部隆起区受扬子板块俯冲改造成类似EM2型;盆地变形的力源为板块相对运动产生的引张力,以及郯庐断裂的走滑作用。新生代,渤海湾盆地以窄裂陷模式伸展,地壳和岩石圈地幔变形方式均为纯剪,但岩石圈地幔伸展强度大于地壳;盆地处于大陆内裂谷环境,软流圈地幔上涌并改造岩石圈地幔,且盆地裂陷的力源以软流圈地幔上涌产生的引张力为主。     

中亚造山带东南部晚古生代-早中生代地壳增生和古亚洲洋演化:来自内蒙古东南部林西-东乌旗地区岩浆岩的证据SCIEI北大核心CSCD

本文在系统收集内蒙古林西-东乌旗地区晚古生代-早中生代岩浆岩的年代学、岩石地球化学以及锆石Hf同位素资料基础上,通过分析岩浆岩岩石组合随时空的变化规律,并结合区域地质资料,探讨了中亚造山带东南部洋盆演化和地壳增生等重要地质问题。研究结果表明,二连浩特-贺根山蛇绿岩带南、北两侧晚古生代-早中生代岩浆岩在年代学上显示不同的活动期次,具有不同岩石组合和地球化学特征,指示它们分属于不同的构造岩浆岩带。蛇绿岩带以北晚泥盆世-中二叠世岩浆活动在时间上呈连续分布的特征,并在晚石炭-早二叠世时期达到活动峰值。火成岩构造组合分析表明,晚泥盆世-石炭纪和早-中二叠世岩浆活动分别与二连浩特-贺根山洋盆向乌里雅斯太大陆边缘之下的俯冲和洋盆闭合后俯冲板片断离引起的软流圈上涌造成的区域伸展背景有关。蛇绿岩带以南岩浆活动时间上呈现石炭纪、早-中二叠世、晚二叠世-三叠纪幕式分布特征,各期岩浆活动前锋有随时间向南迁移的趋势。这三期岩浆活动分别与古亚洲洋板片向宝力道岛弧之下的俯冲、板片后撤以及洋盆消失之后古板块的碰撞造山作用有关。锆石Hf同位素分析表明,中亚造山带东南部晚古生代至早中生代时期存在显著的地壳增生;其中二连浩特-贺根山蛇绿岩带以北表现为地壳的垂向增生,以南表现为地壳的侧向增生。     

雅鲁藏布江缝合带内构造岩片划分及形成——以仲巴-桑桑段为例

构造岩片作为造山带中非史密斯地层地区的填图单位有其重要的地质意义,本文将雅鲁藏布江缝合带分为6大构造岩片,其中蛇绿混杂岩岩片又分4个次级岩片,进一步阐述了缝合带内不同单元具有不同岩性和不同构造型式,是一条复杂的构造带,并发现俯冲板块一侧的不同构造单元具有自南而北,由脆性变形到低温高压变质、脆-韧性变形,超基性岩的深层次韧性变形的分布规律,大多数岩片的分布是通过多重逆冲推覆型或走滑型的断层将其从地壳深部挤出定位的。雅鲁藏布江缝合带内的构造岩片特征,反映了冈瓦那大陆北缘自三叠纪末期到第四纪经历了裂陷、扩张、多岛洋、闭合、俯冲、碰撞、褶皱、推覆造山的全过程。     

板块俯冲对济阳坳陷形成的制约

为了研究地幔柱、西太平洋板块俯冲对济阳坳陷的影响, 在前人提出的地幔柱观点的基础上, 总结济阳坳陷的地质特征及关于地震震源分布与板块俯冲的研究成果, 发现济阳坳陷的沉积地层、岩浆活动、构造拉张、地热梯度、密度流成因的储集砂体由南而北有规律地分布; 俯冲板块进入地幔的过程实际上构成了地幔对流的下降流, 地幔660km (或670km) 深处是俯冲板块进入地幔后地幔物质调整所引发的上升流的深度; 西太平洋板块向下俯冲时下插角度由南而北减小, 俯冲板块到达地震不连续面的时间自南向北增大, 使地幔柱由南向北迁移, 导致济阳坳陷的地质、地球物理特征具有规律分布的特点.      

特提斯地球动力学

特提斯是地球显生宙期间位于北方劳亚大陆和南方冈瓦纳大陆之间的巨型海洋,它在新生代期间的闭合形成现今东西向展布的欧洲阿尔卑斯山、土耳其-伊朗高原、喜马拉雅山和青藏高原。根据演化历史,特提斯可划分为原特提斯、古特提斯和新特提斯三个阶段,分别代表早古生代、晚古生代和中生代期间的大洋。大约在500Ma左右,冈瓦纳大陆北缘发生张裂,裂解的块体向北漂移,并使其与塔里木-华北之间的原特提斯洋在420～440Ma左右关闭,产生原特提斯造山作用,与北美-西欧地区Avalonia地体与劳伦大陆之间的阿巴拉契亚-加里东造山作用基本相当。原特提斯造山带之南、早古生代即已存在的龙木错-双湖-昌宁-孟连古特提斯洋在380Ma向北俯冲,使早期闭合的康西瓦-阿尼玛卿洋重新张开,并由于弧后扩张形成金沙江-哀牢山洋。330～360Ma左右,特提斯西部大洋由于南侧非洲板块和北侧欧洲板块的碰撞而关闭,形成欧洲华力西造山带。而特提斯东段的上述三条古特提斯洋在250Ma左右基本同时关闭,华北、华南、印支等块体聚合形成华夏大陆。该大陆与冈瓦纳大陆、劳亚大陆和华力西造山带一起围限形成封闭的古特提斯残留洋,并一直到晚三叠世-早侏罗世海水才全部退出。此后,南侧冈瓦纳大陆在三叠纪晚期重新裂解形成新特提斯洋,该洋盆在新生代初期由于印度和亚洲的碰撞而关闭。原、古、新特提斯三次造山作用基本代表了中国大陆显生宙期间的地质演化历史,并在此过程中形成了特色的特提斯域金属成矿作用。广布的被动陆缘和赤道附近的古地理位置,以及后期的造山作用同时也成就了特提斯域内巨量油气资源的形成;塑就的地貌与海陆分布格局,也对当时的古气候与古环境产生了重要影响。特别是,与原、古、新特提斯洋消亡相关的三次弧岩浆活动与显生宙地球历史上三次温室地球向冰室地球的转变,在时间上高度吻合。上述演化历史同时还表明,特提斯地质演化以南侧冈瓦纳大陆不断裂解、块体向北漂移并与劳亚大陆持续聚合为特征,其动力机制主要来自俯冲板片的拖拽力,而地幔柱是否对大陆的裂解与漂移有所贡献,则有待进一步评价。     

西昆仑加里东期造山作用初探

在西昆仑前山一带存在一个发育完全的加里东期碰撞造山带，该造山带代表了古秦－－祁－－昆大洋的消亡和两侧大陆的剧烈碰撞，古昆仑洋可能开始裂解于震旦纪，寒武纪达最大程度，奥陶纪开始向南俯冲消减，志留纪两侧陆块发生碰撞。其曼于特－－库地蛇绿岩为其洋壳残片，北侧的塔里木板块南缘具被动边缘性质，南侧的西昆仑地块为活动边缘性质，同时有大量俯冲型，碰撞型和造山期后伸展型花岗岩侵入，晚泥盆世紫红色磨拉石建造代表了这一过程的结束。     

Linking the NE Anatolian and Lesser Caucasus ophiolites: evidence for large-scale obduction of oceanic crust and implications for the formation of the Lesser Caucasus-Pontides Arc

In the Lesser Caucasus and NE Anatolia, three domains are distinguished from south to north: (1) Gondwanian-derived continental terranes represented by the South Armenian Block (SAB) and the Tauride–Anatolide Platform (TAP), (2) scattered outcrops of Mesozoic ophiolites, obducted during the Upper Cretaceous times, marking the northern Neotethys suture, and (3) the Eurasian plate, represented by the Eastern Pontides and the Somkheto-Karabagh Arc. At several locations along the northern Neotethyan suture, slivers of preserved unmetamorphozed relics of now-disappeared Northern Neotethys oceanic domain (ophiolite bodies) are obducted over the northern edge of the passive SAB and TAP margins to the south. There is evidence for thrusting of the suture zone ophiolites towards the north; however, we ascribe this to retro-thrusting and accretion onto the active Eurasian margin during the latter stages of obduction. Geodynamic reconstructions of the Lesser Caucasus feature two north dipping subduction zones: (1) one under the Eurasian margin and (2) farther south, an intra-oceanic subduction leading to ophiolite emplacement above the northern margin of SAB. We extend our model for the Lesser Caucasus to NE Anatolia by proposing that the ophiolites of these zones originate from the same oceanic domain, emplaced during a common obduction event. This would correspond to the obduction of non-metamorphic oceanic domain along a lateral distance of more than 500?km and overthrust up to 80?km of passive continental margin. We infer that the missing volcanic arc, formed above the intra-oceanic subduction, was dragged under the obducting ophiolite through scaling by faulting and tectonic erosion. In this scenario part of the blueschists of Stepanavan, the garnet amphibolites of Amasia and the metamorphic arc complex of Erzincan correspond to this missing volcanic arc. Distal outcrops of this exceptional object were preserved from latter collision, concentrated along the suture zones.     

北秦岭元古代构造格架与演化

秦岭造山带是经历了多阶段的多陆块长期裂解、拼合的复合型造山带。最新的地质、地球化学和同位素年代学综合研究共同揭示沿商丹带分布有中新元古代蛇绿岩,并伴生有与板块俯冲碰撞作用相关的弧后盆地、岩浆弧、高压变质作用,表明北秦岭于中元古代末—新元古代初曾发展成为类似于现代板块构造体制的活动大陆边缘,出现板块向北俯冲消减、弧后盆地的生成和蛇绿岩构造侵位及其后的碰撞造山作用。     

秦岭区前寒武纪构造格局与演化问题探讨

秦岭造山带中夹持大量前寒武纪岩层、地块,筛除后期改造与变位,昨原,它们复杂而多样,不仅是秦岭造山带研究的基础,也是研究早期中国大陆壳形成演化的关键地带。现有的地质、地球化学研究,揭示秦岭区早前寒武纪具非统一多块分离拼合特征,晚期已成为早期化南块的边缘带。中新元古代相应于Ｇｒｅｎｖｉｌｌｉａｎ造山事件和Ｒｏｄｉｎｉａ超大陆全球性构造时期,秦岭区从扩张裂谷系与小洋盆兼杂并存的垂向加积增生构造体制向侧向     

班公湖-怒江带、羌塘地块特提斯演化 与成矿地质背景

孟家屯岩组是山东省地矿局第九地质队张连峰等人１９９２年进行１∶５００００新汶、放城幅区调时，在新泰市孟家屯一带发现的一套石英岩组合的表壳岩，并将其划归为泰山岩群的底部［１］。前人认为孟家屯岩组总体上发生了３期变质作用?：第一期区域变质作用，使孟家屯岩组泥质岩中出现了斜长石、蓝晶石、铁铝榴石，基性岩中出现斜长石、普通角闪石等新生矿物，变质作用达中级变质，岩石的形成温度为T＝５３０～６３０℃，压力p＝０．５８～０．７２GPa，属中压相系中的低角闪岩相；第二期区域变质作用为泰山岩群地层发生的退变质作用，形…     

Subduction of a fossil slow–ultraslow spreading ocean: a petrology-constrained geodynamic model based on the Voltri Massif,Ligurian Alps,Northwest Italy

Slow–ultraslow spreading oceans are mostly floored by mantle peridotites and are typified by rifted continental margins, where subcontinental lithospheric mantle is preserved. Structural and petrologic investigations of the high-pressure (HP) Alpine Voltri Massif ophiolites, which were derived from the Late Jurassic Ligurian Tethys fossil slow–ultraslow spreading ocean, reveal the fate of the oceanic peridotites/serpentinites during subduction to depths involving eclogite-facies conditions, followed by exhumation.

The Ligurian Tethys was formed by continental extension within the Europe–Adria lithosphere and consisted of sea-floor exposed mantle peridotites with an uppermost layer of oceanic serpentinites and of subcontinental lithospheric mantle at the rifted continental margins. Plate convergence caused eastward subduction of the oceanic lithosphere of the Europe plate and the uppermost serpentinite layer of the subducting slab formed an antigorite serpentinite-subduction channel. Sectors of the rather unaltered mantle lithosphere of the Adria extended margin underwent ablative subduction and were detached, embedded, and buried to eclogite-facies conditions within the serpentinite-subduction channel. At such P–T conditions, antigorite serpentinites from the oceanic slab underwent partial HP dehydration (antigorite dewatering and growth of new olivine). Water fluxing from partial dehydration of host serpentinites caused partial HP hydration (growth of Ti-clinohumite and antigorite) of the subducted Adria margin peridotites. The serpentinite-subduction channel (future Beigua serpentinites), acting as a low-viscosity carrier for high-density subducted rocks, allowed rapid exhumation of the almost unaltered Adria peridotites (future Erro–Tobbio peridotites) and their emplacement into the Voltri Massif orogenic edifice. Over in the past 35 years, this unique geologic architecture has allowed us to investigate the pristine structural and compositional mantle features of the subcontinental Erro–Tobbio peridotites and to clarify the main steps of the pre-oceanic extensional, tectonic–magmatic history of the Europe–Adria asthenosphere–lithosphere system, which led to the formation of the Ligurian Tethys.

Our present knowledge of the Voltri Massif provides fundamental information for enhanced understanding, from a mantle perspective, of formation, subduction, and exhumation of oceanic and marginal lithosphere of slow–ultraslow spreading oceans.     

班公湖-怒江带、羌塘地块特提斯演化 与成矿地质背景

早古生代—泥盆纪,研究区沉积环境以陆棚碎屑岩相和碳酸盐台地相为主,代表冈瓦纳大陆北缘和特提斯南侧的被动大陆边缘。石炭纪—二叠纪,本区进入特提斯南、北缘弧盆系统演化阶段,龙木错-双湖带北部、金沙江带南部和冈底斯带分别在石炭纪、二叠纪形成岩浆弧。中生代是特提斯南缘弧盆演化阶段,SSZ型蛇绿岩形成岩浆熔离型铬、镍、铂族金属矿床和热液型金矿。班公湖-怒江带特提斯在中侏罗世至早白垩世向南、北两侧俯冲并形成岩浆弧,该岩浆弧是重要的成矿带,形成斑岩铜矿、矽卡岩型磁铁矿和热液型多金属矿床。北羌塘东段侏罗纪弧后前陆盆地有利于形成沉积型、沉积-热液改造型和热液型铁、铜、锑、金矿床。晚白垩世碰撞作用主要与热液型矿床有关,分布范围较大,也可能存在晚白垩世至新生代碰撞阶段的斑岩铜矿。     

北淮阳构造带的属性及其对板块缝合线位置的启示

北淮阳构造带为一条沿大别造山带北麓展布的狭长构造带,是华北板块与扬子板块碰撞造山的产物,其物源组成、构造属性等研究内容是揭示南北板块在中国东部的大地构造单元格局以及时空演化的关键信息。结合构造变形、岩石学、岩石地球化学、锆石U-Pb年代学等方法对北淮阳前中生代岩石地层单元苏家河群/卢镇关群和信阳群/佛子岭群进行对比分析,就其构造属性形成这样的基本认识:北淮阳构造带是杨子板块向华北板块俯冲-碰撞的结合带,其物质组成具有双源性-主体部分来源于杨子板块,由代表了杨子板块北缘基底的晚元古代苏家河群(784±19Ma)/卢镇关群(756±12Ma)和杨子板块被动陆缘复理石沉积建造-中泥盆世至晚泥盆世早期的信阳群南湾组组成,后者相当于商丹缝合带以南的刘岭群;信阳群龟山组亲缘于华北板块并构成华北板块南缘的弧前楔形沉积体,是沿商丹缝合带分布的桃花铺弧前楔形沉积体的东延。佛子岭群总体可与信阳群相连,全岩成分显示,佛子岭群沉积构造环境既有活动大陆边缘,又有被动大陆边缘。由于中生代以来多期构造变形叠加(至少三期),佛子岭群岩石地层单元的叠置关系被改造或重置,使其缺少"构造解体"的证据,而无法在构造单元上细分。对于两大板块之间的缝合带位置,笔者认为:商丹缝合带进入北淮阳构造带后,应沿着北淮阳的北界,与龟山-梅山-六安-磨墩水库一线延伸的断裂带相连。     

祁连山蛇绿岩带和原特提斯洋演化

位于阿拉善地块和柴达木地块之间的祁连造山带记录原特提斯洋扩张、俯冲、闭合、大陆边缘增生和碰撞造山的完整过程。从南向北,祁连造山带发育有三条平行排列、不同类型的蛇绿岩带:(1)南部南祁连洋底高原-洋中脊-弧后蛇绿岩混杂带;(2)中部托勒山洋中脊型蛇绿岩带;(3)北部走廊南山SSZ型蛇绿岩带。南部南祁连蛇绿混杂岩带以拉脊山-永靖蛇绿岩为代表,为典型的洋底高原型蛇绿岩,是大洋板内地幔柱活动的产物,形成年龄为525～500Ma;中部托勒山蛇绿岩带沿熬油沟-玉石沟-冰沟-永登一线分布,为大洋中脊型蛇绿岩,蛇绿岩形成年龄为550～495Ma;北部蛇绿岩带包括弧前和弧后两种类型,弧前蛇绿岩以大岔大阪蛇绿岩为代表,形成时代为517～487Ma,反映初始俯冲/弧前扩张到弧后盆地的过程;弧后蛇绿岩以九个泉-老虎山蛇绿岩为代表,为典型的SSZ型蛇绿岩,是弧后扩张的产物,形成时代为奥陶纪(490～445Ma)。三个蛇绿岩带分别代表了新元古代-早古生代祁连洋演化历史不同环境的产物,对了解秦祁昆构造带原特提斯洋的构造演化过程有重要意义。蛇绿岩及弧火山岩的时空分布特征限定了原特提斯洋的俯冲极性为向北消减俯冲。     

大别-苏鲁造山带的东延及板块缝合线:郯庐-鸭绿江-延吉断裂的厘定

根据大别-苏鲁造山带北缘和吉林-黑龙江东部的三叠纪浅变质加积杂岩特征标志,认为大别地区的板块缝合线为信阳-舒城断裂,苏鲁地区的为郯庐-鸭绿江断裂,且苏鲁造山带向北延入东北的吉林-黑龙江东部地区,而华北与扬子板块之间构造缝合线的东延部分则为郯庐-鸭绿江-图们江-延吉断裂。在此基础上,提出了亚洲东部三叠纪以来连续的俯冲-加积模型：(1)三叠纪扬子板块在华北板块向南突出部位(大别-苏鲁一带)发生点碰撞形成超高压变质岩,之后扬子板块由点碰撞逐渐向两侧旋转拼贴形成加积杂岩;(2)侏罗纪-新生代在三叠纪碰撞基础上,太平洋板块向欧亚大陆连续俯冲和加积,进而形成由三叠纪-新生代杂岩组成的欧亚大陆东部地区的巨大加积杂岩带。     

珠江口盆地构造演化旋回及其新生代沉积环境变迁

目前对珠江口盆地中生代以来的演化过程及其与沉积环境演变的响应关系尚缺乏系统性认识.基于珠江口盆地中-新生代岩浆活动、断陷结构样式及其改造、典型构造变形样式、沉积中心的转换等特征的对比分析,将盆地中-新生代的构造演化划分为4个阶段、7个期次：（1）中侏罗世-晚白垩世早期（～170～90 Ma）为古太平洋板块俯冲主控的陆缘岩浆弧-弧前盆地演化阶段;（2）晚白垩世-始新世中期（～90～43 Ma）为太平洋板块俯冲后撤背景下弧后周缘前陆/造山后塌陷-主动裂谷演化阶段;（3）始新世中期-中中新世（～43～10 Ma）为华南挤出-古南海俯冲拖曳主导的被动陆缘演化阶段;（4）晚中新世以来（～10～0 Ma）为菲律宾板块NWW向仰冲主导的挤压张扭演化阶段.～90 Ma、～43 Ma、～10 Ma分别实现了由安第斯型俯冲向西太平洋型俯冲、由主动裂谷向被动陆缘伸展、由被动陆缘伸展向挤压张扭的转换.在此过程中,伴随着古南海和南海的发育-消亡,新生代裂陷期沉积环境由东向西、由南向北逐渐海侵,裂后期由南向北阶段性差异沉降,由陆架浅水向陆坡深水转换,这使得珠一/三、珠二、珠四坳陷的石油地质条件具有显著的分带差异性...