共查询到20条相似文献，搜索用时 15 毫秒
1.
E. A. Toto A. El Miloudi M. El Basri M. Hafid L. Zouhri S. El Mouraouah M. Benammi A. El Mouraouah A. Iben Brahim A. Birouk M. Kasmi 《Environmental Earth Sciences》2012,67(8):2411-2422
Combining the results from field observations, high resolution 2D-electric resistivity and high resolution seismic refraction tomography, we have found new evidence for active faulting in the Dhar Doum area, northwestern Atlantic coast of Morocco. Qualitative interpretation of the inverted resistivity and seismic refraction data reveals the presence of two thrust faults that cut the topographic surface and displace the most recent sedimentary deposits. Furthermore, one of these seismically imaged faults strongly correlates with the Dhar Doum?CLalla Zahra fault. The steepening at the surface and the flattening with depth of this fault are likely to indicate an important strike-slip component associated with a major reverse component. If extended offshore to the west, the Dhar Doum fault could be a continuation of the southernmost deformational front of the Cadiz oceanic accretionary prism. Therefore, this structure is very likely to represent the actual active southern deformational front of the oceanic accretionary prism, as well as that of the Rif fold-and-thrust belt. The southward thickening of the growth strata composing the uppermost dune system and the occurrence of Plio-Quaternary conglomerates north of the Dhar Doum?CLalla Zahra fault suggest that the neotectonic activity may have started by the end of the Pliocene and have continued to the present as indicated by the folding-and-faulting of the most recent sedimentary deposits and the presence of high scarps. The identification of active faulting in the study area that may have a profound influence on seismic hazard analysis of the whole Rif foredeep basin. 相似文献
2.
The Gulf of Cadiz spans the plate boundary between Africa and Eurasia west of the Betic-Rif mountain belt. A narrow east dipping subduction zone descends beneath the Gulf of Cadiz and the straits of Gibraltar. The deep crustal structure of the Gulf and the adjacent SW Iberian and Moroccan margins is constrained by numerous multi-channel seismic reflection and wide-angle seismic surveys. A compilation of these existing studies is presented in the form of depth to basement, sediment thickness, depth to Moho and crustal thickness maps. These structural maps image an E-W trending trough, with thin (< 10 km) crust beneath the Gulf of Cadiz. This trough is filled by an eastward thickening wedge of sediments, reaching a thickness of 10-15 km in the eastern Gulf. These sediments are tectonically deformed, primarily along a series of westward-vergent thrust faults and represent a 200-250 km wide accretionary wedge. The northern and especially the southern limits of the accretionary wedge are marked by sharp morphological lineaments showing evidence of recent deformation. These tectonic limits are situated in an internal position with respect to the Miocene deformation front (external Betic and Rif allocthons), which has been abandoned. At the western boundary of the accretionary wedge, near the adjacent Seine and Horseshoe abyssal plains, an E-W trending basement high (Coral Patch Ridge) can be seen indenting the deformation front in an asymmetric manner. Analog modeling is performed using granular materials accreted against a semicircular backstop (representing the basement of the Rif and Betic mountain belts). The modeling initially produces a symmetric, arcuate accretionary wedge. The ensuing collision of an oblique rigid indenter retards accretion on one side, resulting in an embayment and a locally steeper deformation front. The deformation pattern observed in morphology and high-resolution seismic profiles suggests the accretionary wedge and underlying subduction system is still active. The implications of active subduction for the source region of the 1755 Lisbon earthquake and the regional seismic hazard assessment are discussed. 相似文献
3.
The Lachlan Transverse Zone is a major yet subtle west‐northwest‐trending structure that cuts across the Tasmanides of southeastern Australia. It extends from the western part of the Olepoloko Fault in the west, where it marks the boundary between the Delamerian and Thomson Orogens, across the Lachlan Orogen into the Sydney Basin where it is represented by dykes and intrusions. The western part of the Lachlan Transverse Zone is defined by west‐northwest‐trending faults. In the Eastern Belt of the Lachlan Orogen, it is defined as a corridor of west‐northwest‐trending folds and faults that disrupt major folds and faults which constitute the regional grain of the orogen. The Lachlan Transverse Zone was active in the development of the Lachlan Orogen since at least the Middle Ordovician period. It has influenced the partitioning of upper crustal extensional and contractional deformation, the intrusion of igneous bodies as well as the distribution of copper‐gold deposits in the Eastern Belt of the orogen. The Lachlan Transverse Zone appears to be an extension of the Proterozoic Amadeus Transverse Zone, as well as an extension of a west‐northwest‐trending transform segment in the Tasman Line that controlled the Neoproterozoic and Cambrian breakup of cratonic Australia. For these reasons, we suggest that the Lachlan Transverse Zone represents the reactivation of a fundamental crustal weakness in the cratonic lithosphere that propagated into younger Neoproterozoic to Palaeozoic lithosphere of oceanic and continental character. 相似文献
4.
Structural trends in the Celtic Sea area indicate that Variscan deformation patterns were inherited from Caledonian basement structures, and that the regional fold alignment is arcuate with a regional WSW-ENE direction rather than WNW-ESE (Armorican). There is no lateral structural continuity between Southern Ireland and South Wales-Southwest England. Three major structural provinces arranged en échelon across the Variscan foldbelt are recognised: (a) Southwest England, where there was complex deformation of a major basin; (b) the South Wales-Mendips foreland area, with strong basement/cover interaction and (c) the Southern Ireland graben and flanking platform province. Late Palaeozoic depositional patterns indicate that Southern Ireland and Southwest England were separated by a WSW-ENE trending platform bounded on the north by the inherited Wexford Boundary Lineament and to the south by a previously unidentified major Palaeozoic fault zone, here termed the Bristol Channel Lineament. The South Wales-Mendips Variscan successions accumulated on this intervening Wales-Celtic Sea platform, and were partly influenced by rejuvenated Caledonian fault lines. It is suggested that the northern margin of the Rheno-Hercynian foldbelt (the Variscan Front) be taken along the Bristol Channel Lineament, which can be traced for some 400 km southwestwards towards the Goban Spur on the continental margin. This permits a rationalisation of both tectonic and major facies boundaries in locating the front. It is also suggested that the structurally localised nature of the Southern Ireland basin be recognised by designating it as the Southern Ireland Zone of the Variscan foldbelt.The sites of Mesozoic rifting in the Celtic Sea and adjacent areas, although complex in detail, appear to have been located along the Wexford Boundary and Bristol Channel Lineaments. 相似文献
5.
鄂尔多斯盆地西缘位于华北陆块和秦祁昆山造山带两个一级大地构造单元之间的过渡带内,特定的大地构造背景使其具有复杂的构造演化历程及特殊的煤田构造格局。鄂尔多斯盆地西缘由贺兰山逆冲推覆构造系统和六盘山东麓逆冲推覆构造系统组成,具有"南北分段、东西分带"的特点。为了进一步探讨鄂尔多斯盆地西缘煤田构造格局的形成演化及区域构造控制因素,本文基于野外地质调查和煤田勘查资料,恢复了本区自晚古生代以来的沉降抬升史和古构造应力场特征。印支期:研究区北部最大主压应力方向为北西-南东向,南部最大主压应力方向为北东-南西向;燕山期:北部最大主压应力方向为北西西-南东东向,南部最大主压应力方向为北东东-南西西向;喜马拉雅山期:北部受北西西-南东东向拉张应力,南部最大主压应力方向为北东-南西向。采用有限元数值模拟,探讨了鄂尔多斯盆地西缘煤田构造格局的形成与区域构造的演化的关系,强调北段贺兰山逆冲推覆构造系统的形成与阿拉善地块的向东挤出逃逸密切相关。 相似文献
6.
辽宁省金矿集中区及其与构造样式的关系 总被引：1，自引：0，他引：1
本文将辽宁省金矿划分四种类型,十个主要金矿集中区。这些集中区均受华北地台东西向基底构造活动带及中生代太平洋板块俯冲影响、所产生的北西向构造挤压带和北东向构造—岩浆岩带的复合作用控制。它们分别处于太不洋成矿带的内带(辽东)和外带(辽西)。并以郯庐断裂为轴线,构成了两大“U”字形,类似共轭曲线展布的构造样式。根据深部地球物理资料,综合分析了控制金矿集中区构造样式的形成机制。区内脉状金矿大都分布在深断裂(深度大于五公里断裂)带附近。 相似文献
7.
A. H. M. VandenBerg A. C. Sandford R. B. Rickards 《Australian Journal of Earth Sciences》2013,60(4):659-665
The Kambalda Ni province, located in the Archaean Norseman‐Wiluna greenstone belt of Western Australia, boasts the largest known concentration of komatiite‐associated magmatic Fe–Ni–Cu sulfide deposits. These are found as long, linear massive to disseminated bodies at the base of a thick komatiite sequence. The sulfide bodies are closely associated with, or contained within, trough structures at the contact with the underlying basaltic unit. In this study, the McComish Prospect, located 40 km south of Kambalda at Tramways, was studied to assess the relationships between volcanic facies, mineralisation and trough structures. The rocks in this region have variably experienced four phases of deformation, upper greenschist ‐ lower amphibolite facies metamorphism, granitoid intrusion, and subsequent alteration. Relict igneous textures are locally preserved at McComish, however, enabling the evaluation of existing geological models and interpretations. The McComish trough is considered to be entirely structural in origin and unrelated to primary volcanic processes (e.g. thermal erosion). The association of volcanic textural facies in individual flow units, and the distribution of flow units across the trough is more complex than predicted by prevailing models, suggesting an alternative komatiite lava emplacement mechanism. Results are consistent with the proposal that komatiites did not flow turbulently as widely accepted, nor did they cool by vigorous convection. Alternatively, the lavas were emplaced as inflated, lobate basalt pahoehoe‐like flows. Although Fe–Ni–Cu sulfide mineralisation at McComish is most likely volcanic in origin, its present distribution appears to be structurally controlled or modified. The zone of weakly to strongly disseminated sulfides at the base of the komatiite sequence is thickened adjacent to a major north‐northwest‐trending fault on the western margin of the trough. This fault is interpreted to have been a fluid conduit, remobilising the ore during metamorphism and deformation. 相似文献
8.
黔西北五指山地区叠加构造变形特征对铅锌矿成矿的控制 总被引：1，自引：0，他引：1
五指山铅锌矿区位于贵州省普定县与织金县交界区域,大地构造位于扬子板块中部、江南造山带西缘。野外构造研究表明,受早古生代加里东构造运动的控制与影响,矿区内震旦系—下古生界构造变形与上古生界—中生界的构造变形明显不同。震旦系—下古生界构造线近东西向,发育近东西向平缓褶皱、南倾或北倾劈理,显示近南北向的挤压收缩变形。震旦系—下古生界区内发育两组南北、北西向陡倾断层,断层明显受限制而不穿越晚古生代之后的地层。发育在震旦系—下古生界内的层间滑动与断层活动控制着铅锌矿的分布。晚古生代之后区域构造应力场发生转变,由早期近南北向的挤压收缩转为早燕山期SEE向NWW挤压逆冲,由此对震旦纪—早古生代变形进行叠加与改造,宏观上形成以NE走向为特征的区域构造格局。后期形成的褶皱轴面主要向SEE倾斜,断层向NWW逆冲,与早期变形呈斜跨式叠加。燕山期断层活动促进了铅锌矿的迁移与聚集。 相似文献
9.
《Geodinamica Acta》2013,26(5-6):231-238
Reprocessing and interpretation of the petroleum seismic profile 81SE5b, located between the Luberon Massif and the Arc Basin, have provided new data on the Pyrenean and Alpine thrusting in western Provence. Among the principal results, it is shown that a) the repetition of the Mesozoic succession observed in the Eguilles1 borehole is due to a north-dipping south-verging thrust, and b) the Trévaresse and Aix-Eguilles thrusts are deep structures rooted in the Triassic at a depth of between 7 and 8 km. The implication of this new knowledge on the seismotectonic model of western Provence is that the front of the Alpine deformation between the Aix-en-Provence and Salon-Cavaillon fault systems, which acted as lateral ramps, lies some 7 km farther south near the northern limb of the Arc syncline. In addition, it is seen that the Alpine-Provence thrusts, considered as still active (having given rise to the 1909 earthquake with an epicentral intensity of VIII-IX), are not shallow reverse faults but correspond to major tectonic structures affecting the full thickness of the Meso-Cenozoic cover. 相似文献
10.
该区的构造格局主要由早期近东西向紧闭的褶皱带和晚期北北东向构造组成。早期的南北向缩短构造以龙王庙平卧褶皱和大小长山岛的直立紧闭褶皱为代表,分别具有扇状间隔性压溶劈理和透入性轴面片理,褶面倒向以北为主。北北东向构造切割近东西向构造,表层表现为北西西向薄皮逆冲推覆构造,浅层构造具有扇状压溶劈理的紧闭褶皱,深层表现为基底与盖层间的拆离断层及其下的韧性剪切带。早期的研究者将该断层作为辽南推覆构造底部的滑脱面,现今则压倒性地采用变质核杂岩的构造理念。根据相关剪切带早期面内褶皱发育,晚期伸展褶劈理发育,通过运动学涡度和应力状态分析,论证早期滑脱-推覆到晚期伸展拆离的演化过程。野外观测证明,辽南基底变质岩西侧的金州断层为一伸展拆离断层,它切割东侧的董家沟断层,前者平行于下伏糜棱岩中的同向伸展褶劈理,后者平行下伏糜棱岩的糜棱面理。金州拆离断层的形成及其东侧的隆起标志着辽南构造体制从缩短到伸展的转折。根据相关的年代学研究,这一构造体制转化发生在早白垩世(约120～107 Ma)。该区最新的构造事件是北东-南西向的缩短,相关的北北东向的右行走滑断层与晚白垩世以来的郯庐断层活动方式一致。 相似文献
11.
遥感蚀变信息定量提取方法在成矿预测中的应用——以西昆仑塔什库尔干地区为例 总被引：4，自引：3，他引：1
以遥感技术为手段、ETM影像为基础数据,解译了西昆仑塔什库尔干地区主要线、环构造,划分出北西、近南北和近东西向3组主要线性断裂.利用比值和主成分分析等方法,通过异常下限值圈定的数学模型定量提取了铁化、泥化和硅化蚀变信息.综合分析地质、矿产、地球化学及物、化探异常等资料,结合遥感构造解译和蚀变信息,优选了2个Ⅰ类找矿靶区... 相似文献
12.
Naoko Kato Hiroshi Sato Masayuki Orito Kazuomi Hirakawa Yasutaka Ikeda Tanio Ito 《Tectonophysics》2004,388(1-4):75
A NS trending Cenozoic fold-and-thrust belt has developed in the western part of the Hidaka Collision Zone (HCZ), central Hokkaido, Japan. A quantitative estimation of the late Cenozoic convergence rate at the front of the Hidaka thrust system is important in revealing the plate tectonic framework around northern Japan. High-resolution seismic reflection profiling across the active fault-related folds was carried out to ascertain the temporal change in the crustal shortening rate. Overlapping ramp anticlines and growth folds within thrust sheets were examined using balanced cross-sections combined with industry seismic and drilling data. The rate of shortening was examined using a 3.5 Ma horizon and late Quaternary horizons at 115 and 41 ka. These horizons show that the convergence rate of the Hidaka thrust system has not decreased during the last 3.5 Ma. This suggests that the plate boundary between the Eurasian (Amurian) and North American (Okhotsk) plates has not jumped from the central part of Hokkaido to the eastern part of the Sea of Japan since 3.5 Ma and that a significant amount of plate convergence is still being absorbed in the Hidaka Collision Zone. 相似文献
13.
《Journal of Asian Earth Sciences》1999,17(1-2):99-122
The Barito, Kutei, and Tarakan Basins are located in the eastern half of Kalimantan (Borneo) Island, Indonesia. The basins are distinguished by their different tectonic styles during Tertiary and Pleistocene times. In the Barito Basin, the deformation is a consequence of two distinct, separate, regimes. Firstly, an initial transtensional regime during which sinistral shear resulted in the formation of a series of wrench-related rifts, and secondly, a subsequent transpressional regime involving convergent uplift, reactivating old structures and resulting in wrenching, reverse faulting and folding within the basin. Presently, NNE–SSW and E–W trending structures are concentrated in the northeastern and northern parts of the basin, respectively. In the northeastern part, the structures become increasingly imbricated towards the Meratus Mountains and involve the basement. The western and southern parts of the Barito Basin are only weakly deformed. In the Kutei Basin, the present day dominant structural trend is a series of tightly folded, NNE–SSW trending anticlines and synclines forming the Samarinda Anticlinorium which is dominant in the eastern part of the basin. Deformation is less intense offshore. Middle Miocene to Recent structural growth is suggested by depositional thinning over the structures. The western basin area is uplifted, large structures are evident in several places. The origin of the Kutei structures is still in question and proposed mechanisms include vertical diapirism, gravitational gliding, inversion through regional wrenching, detachment folds over inverted structures, and inverted delta growth-fault system. In the Tarakan Basin, the present structural grain is typified by NNE–SSW normal faults which are mostly developed in the marginal and offshore areas. These structures formed on older NW–SE trending folds and are normal to the direction of the basin sedimentary thickening suggesting that they developed contemporaneously with deposition, as growth-faults, and may be the direct result of sedimentary loading by successive deltaic deposits. Older structures were formed in the onshore basin, characterized by the N–S trending folds resulting from the collision of the Central Range terranes to the west of the basin. Hydrocarbon accumulations in the three basins are strongly controlled by their tectonic styles. In the Barito Basin, all fields are located in west-verging faulted anticlines. The history of tectonic inversion and convergent uplift of the Meratus Mountains, isostatically, have caused the generation, migration, and trapping of hydrocarbons. In the Kutei Basin, the onshore Samarinda Anticlinorium and the offshore Mahakam Foldbelt are prolific petroleum provinces, within which most Indonesian giant fields are located. In the offshore, very gentle folds also play a role as hydrocarbon traps, in association with stratigraphic entrapment. These structures have recently become primary targets for exploratory drilling. In the Tarakan Basin, the prominent NW–SE anticlines, fragmented by NE–SW growth-faults, have proved to be petroleum traps. The main producing pools are located in the downthrown blocks of the faults. Diverse tectonic styles within the producing basins of Kalimantan compel separate exploration approaches to each basin. To discover new opportunities in exploration, it is important to understand the structural evolution of neighbouring basins. 相似文献
14.
闹阳坪锌萤石矿床位于北大巴山逆冲推覆褶皱带平利隆起东侧,为该区首次发现的受构造裂隙控制的气水–热液型锌萤石矿床。本文从矿区断裂入手,通过对该区矿床地质、断裂特征、矿体特征的研究,总结了该区断裂的演化序列及其对成矿的控制机制与规律。认为NW-SE向断裂组是矿区的主要控矿构造,矿区断裂变形发育演化序列为晚印支–早燕山期形成近EW向断裂F1,早燕山期形成NW-SE向断裂F7和NE-SW向断裂F4,随后的右行走滑作用叠加有张扭性应力,形成有利于成矿热液运移充填成矿的张扭性右行走滑断裂。并明确了成矿期应变椭球体,恢复了成矿期主压应力方向为NNW向(340°~350°)。在此基础上,预测平面上闹阳坪矿区F7与F8断裂之间为下一步找矿重点地段,剖面上K3萤石矿体下伏北东方向可能存在隐伏矿体。 相似文献
15.
16.
Ines Ezzine Mohammed Jaffal Fouad Zargouni Mohamed Ghanmi 《Arabian Journal of Geosciences》2011,5(5):1117-1125
A residual anomaly gravity map of the Maktar area has been processed via several methods including horizontal gradient, upward continuation, and Euler deconvolution to highlight structures hidden by sedimentary cover. These methods reinforce the existence of several faults inferred from geologic studies. This work outlines deep or near-surface faults that had remained hidden until now. The most important set of these faults is NE–SW trending, with depths in excess of 3,000 m. These faults limit the Northwestern limb of Balouta massif and restrain the Northwestern side of Oued Ousafa syncline. This last fault presents a thrust front which constituted the western continuity of a southern Tunisian thetys margin and a western Zaghouan scar prolongation. E–W striking faults refer to an arched beam of faults limiting Kessera plateau and others situated in the northern part of the Maktar plateau. N–S and NW–SE directions correspond to branches of less-apparent importance. Superposition of local maxima specifies dipping vergence of different proven structures. Results from this work show the importance of gravimetric data analysis in Maktar area and provide new insight into Central Atlas Tunisia structure such as new emergent segment front Alpine chain. The proposed map could be a basis for planning future hydrogeological and petroleum research in this region. 相似文献
17.
《Geodinamica Acta》2003,16(2-6):131-147
Combining fieldwork and surface data, we have reconstructed the Cenozoic structural and tectonic evolution of the Northern Bresse. Analysis of drainage network geometry allowed to detect three major fault zones trending NE–SW, E–W and NW–SE, and smooth folds with NNE trending axes, all corroborated with shallow well data in the graben and fieldwork on edges. Cenozoic paleostress succession was determined through fault slip and calcite twin inversions, taking into account data of relative chronology. A N–S major compression, attributed to the Pyrenean orogenesis, has activated strike-slip faults trending NNE along the western edge and NE–SW in the graben. After a transitional minor E–W trending extension, the Oligocene WNW extension has structured the graben by a collapse along NNE to NE–SW normal faults. A local NNW extension closes this phase. The Alpine collision has led to an ENE compression at Early Miocene. The following WNW trending major compression has generated shallow deformation in Bresse, but no deformation along the western edge. The calculation of potential reactivation of pre-existing faults enables to propose a structural sketch map for this event, with a NE–SW trending transfer fault zone, inactivity of the NNE edge faults, and possibly large wavelength folding, which could explain the deposit agency and repartition of Miocene to Quaternary deformation. 相似文献
18.
阿尔泰山活动断裂 总被引：13，自引：0，他引：13
文中介绍了位于亚洲腹地阿尔泰山地区的活动断裂。中国阿尔泰山 (阿尔泰山西南麓 )和蒙古阿尔泰山 (阿尔泰山的东麓 )以NNW向大型走滑断裂为主 ,科布多断裂是阿尔泰山东麓的一条主要NNW向走滑断裂 ,长度近 70 0km。第四纪中晚期右旋走滑速率可达 6 10mm/a ,其上发现有长逾2 0 0km的古地震形变带。富蕴断裂则是阿尔泰山西南麓的一条主要NNW向断裂 ,中晚第四纪的走滑运动速率为 (4± 2 )mm/a ,在中国阿尔泰山的西端还发育规模相对较小的NNW向右旋走滑断裂 ,中晚第四纪走滑速率为 (2± 1)mm/a。中国阿尔泰山 (阿尔泰山的西南麓 )还发育NWW向右旋走滑逆断裂 ,其规模相对较小 ,至中国阿尔泰山西端NWW向的额尔齐斯断裂具有明显的右旋走滑性质。蒙古阿尔泰山的南端则发育近东西向的左旋走滑逆断裂。在与戈壁阿尔泰山交汇部位 ,左旋走滑运动具主导作用。戈壁阿尔泰山发育的戈壁阿尔泰断裂带断续延伸可达 10 0 0km以上 ,目前的研究认为 ,其滑动速率为 12mm/a。其中的博格德断裂上 195 7年发生了戈壁阿尔泰 8.3级地震 ,形变带长约 2 5 0km。阿尔泰山活动断裂的规模、运动强度和强地震活动表明这里不仅受到遥远的印度板块北向推挤作用的影响 ,而且受到较近的地球动力学过程的影响或控制。 相似文献
19.
海拉尔盆地是叠置于内蒙-大兴安岭古生代碰撞造山带之上的中、新生代盆地,乌尔逊凹陷是海拉尔盆地中部的1个二级构造单元,自早白垩世开始,经历了3次伸展作用、2次挤压作用,盆地中地层厚度和沉降中心的迁移主要受同生断层和与之伴生的断层相关褶皱所控制。在伸展作用时期：当发育1个犁式正断层,在其上盘形成1个箕状断陷,沉降中心位于断层上盘、靠近断层的区域,在伸展量较大的部位形成1个或多个沉降中心;当发育多个控陷正断层,在其上盘形成多个相互独立的箕状断陷,但每一个断陷都有各自的沉降中心,不同方向断层的交汇部位往往就是断陷的沉降中心。随着伸展量的增大,断陷的沉降中心不断向控陷正断层滑动的相反方向迁移,盆地的规模也随之增大。在第一次挤压作用中,早期NS向控陷断层F1发生反转作用,其上盘靠近断层的部位发生隆升,远离断层的部位作为大型断层传播褶皱背斜前翼也发生旋转式隆升,乌尔逊凹陷成为NS向大型断层传播褶皱背斜的前翼向斜,地层的沉积厚度在靠近断层的部位和远离断层的部位都很薄;向大型断层传播褶皱背斜前翼向斜部位,地层的沉积厚度逐渐增大,盆地的沉降中心向向斜的低洼区域迁移。在第二次挤压作用中,早期NS向控陷断层F2发生反转作用,在乌尔逊凹陷中部形成1个规模较大的NS向断层传播褶皱背斜或突发构造,背斜或突发构造的顶部被剥蚀,盆地的沉降中心位于中部背斜带前、后翼向斜的低洼区域。 相似文献
20.
雅布赖含油气盆地位于中国西部河西走廊地区北部,处于华北克拉通阿尔善地块中南部过渡带,属北祁连构造带,中生代为走滑拉分盆地,新生代为挤压冲断坳陷盆地。燕山早期,形成东西向雅布赖拉张断陷,主控断裂为北大山正断层,沉积中心位于盆地南部;燕山中期,碰撞造山作用致使盆地北部急剧抬升,北部中-下侏罗统地层遭受强烈剥蚀;燕山晚期,阿拉善地块及其北部地区处于伸展构造环境,雅布赖山前产生东西向正断层,急剧活动,快速沉降,形成了北东向展布的新的拉张断陷盆地。喜马拉雅期,在挤压走滑作用下,雅布赖盆地南部形成北西向南倾逆冲的推覆构造,致使北大山正断层发生错断瓦解,最终形成"东隆西坳,南断北超"的挤压坳陷构造格局。雅布赖盆地主体沉积凹陷具有较强分割性,沉降凹陷分布于南部,最大沉积岩厚度为5 400 m;凹陷内侏罗系最为发育,中侏罗统新河组、青土井组暗色泥岩、煤岩为烃源岩,砂岩为储集层,新河组泥岩互层作盖层,构成盆地内最主要的含油气组合。由于雅布赖盆地特定的早期深埋,晚期抬升破坏构造格局,造就侏罗系砂岩储层早期强烈压实致密,侏罗系煤系烃源岩成熟较晚,构造发育期与烃源岩排烃期不匹配,生成油气主要表现为近源成藏与层内滞留,形成源内自生自储,致密油应是主要勘探对象。 相似文献