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Layered Tectonics and Mathematical Modeling of the Geodynamic Setting of the Fergana Depression (Uzbekistan) 费尔干纳凹陷(乌兹别克斯坦)的层状构造和地球动力环境数学建模
IF 1.1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-06-19 DOI: 10.1134/s0016852124700043
I. U. Atabekov, Yu. M. Sadykov, J. K. Mamarakhimov

Abstract

The geodynamic features of the Fergana intermontane depression are the presence of rifting during regional meridional compression and the discrepancy between the location of earthquake sources and boundaries of inhomogeneities in crustal layers. The first feature is solved using the ideas of multistage plate tectonics, which also makes it possible to assess the oil and gas content of the basin. However, existing hypothetical tectonic schemes are not supported by mathematical calculations. To clarify these features, we have developed a mathematical model of the stress–strain state with respect to one of the cross sections of the crust in the Fergana depression, which has a zonally inhomogeneous density structure. The results of the mathematical model show that the presence of blocks with different densities creates displacements under the impact of horizontal compressive stresses. It is also shown that the isolines of maximum tangential stresses are located close to the boundaries of inhomogeneous zones, which indicates large errors in determining earthquake hypocenters.

摘要 费尔干纳山间凹陷的地球动力学特征是区域经向压缩过程中存在断裂,以及地震源位置与地壳层不均匀性边界之间存在差异。利用多阶段板块构造学的观点解决了第一个问题,这也使得评估盆地的石油和天然气含量成为可能。然而,现有的假设构造方案并没有数学计算的支持。为了澄清这些特征,我们针对费尔干纳凹陷地壳的一个横截面,建立了一个应力-应变状态数学模型,该横截面具有带状不均匀密度结构。数学模型的结果表明,不同密度块体的存在会在水平压应力的影响下产生位移。结果还表明,最大切向应力的孤立线位于非均质区的边界附近,这表明在确定地震次中心时存在较大误差。
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引用次数: 0
Arc Tectonic Elements and Upper Mantle Structure of Central and Southeast Asia: Seismic Tomography and Seismicity Data 中亚和东南亚的弧形构造要素和上地幔结构:地震层析成像和地震数据
IF 1.1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-06-19 DOI: 10.1134/s001685212470002x
S. Yu. Sokolov, V. G. Trifonov

Abstract

Analysis of the upper mantle plumes spatial distribution in the inner part of the Sunda arc shows a number of plume bodies interrupting the stagnant slab framed from the south by the sinking slab of the Sunda arc. Possible mechanisms resulting in this structure of the mantle are (i) W-E-trending toroidal mantle flow through a gap in a flat slab and (ii) rollback capable of forming a gap in a flat slab and launching upper mantle plumes in it without deep (>1000 km) roots. The space above the top of the slab consists of local hot mantle bodies, which are considered secondary plumes and often form local rift segments. The 3D visualization of velocity variations δVp in the Tibet and Central Asia region demonstrates structural patterns similar to those in the Sunda arc area. One can observe a region of subhorizontal slab fragments and a gap, which is recorded by plume anomalies of deep and secondary origin. The motion vectors of the rock mass along the fault planes of the Sunda arc, detected from seismic events, are directed outward from its center of curvature, in which secondary upper mantle plumes are concentrated. This indicates the development of thrust processes at the arc front unassociated with the subducting plate. The arc thrusting is accompanied by a small number of displacements along antithetic thrust faults. The displacement azimuths along the Himalayas are fan-shaped, oriented toward Hindustan. This shows that the main indicator of tectonic activity (seismic events) has a direction of rock mass displacement to the south from the extensional back-arc basin within Tibet with the development of thrust deformations during movements along the detachment planes. Two directions of seismic movements are distinguished in the Himalayan arc, as well as in the Sunda arc. The first direction follows the Indian Plate subduction model. The second direction includes variable azimuth rock mass movements along the thrust planes onto the Indian Plate.

摘要 对巽他弧内部上地幔羽流空间分布的分析表明,在巽他弧下沉板块从南面框定的停滞板块中,有许多羽流体。造成这种地幔结构的可能机制是:(i) W-E 向环状地幔流穿过平板坯的缝隙;(ii) 回滚能够在平板坯上形成缝隙,并在其中释放上地幔羽流,而没有深根(>1000 公里)。板顶上方的空间由局部热地幔体组成,这些热地幔体被认为是次级羽流,通常形成局部裂谷段。西藏和中亚地区速度变化 δVp 的三维可视化显示了与巽他弧地区类似的结构模式。我们可以观察到一个由亚水平板块碎片和缝隙组成的区域,该区域被深层和次生羽状异常所记录。从地震事件中探测到的沿巽他弧断层面的岩块运动矢量是从其曲率中心向外的,次生上地幔羽流集中于此。这表明弧前推力过程的发展与俯冲板块无关。伴随着弧形推力的是沿反向推力断层的少量位移。喜马拉雅山脉沿线的位移方位角呈扇形,朝向印度斯坦。这表明,构造活动(地震事件)的主要指标是从西藏境内的伸展型弧后盆地向南发生岩体位移的方向,并在沿剥离面运动的过程中产生了推力变形。喜马拉雅弧和巽他弧的地震运动有两个方向。第一个方向遵循印度板块俯冲模式。第二个方向包括沿推力平面向印度板块的可变方位角岩块运动。
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引用次数: 0
Influence of Modern Geodynamic Processes on the Formation of the Coastal Relief and Seabed of the White Sea 现代地球动力过程对白海沿岸地形和海底形成的影响
IF 1.1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-06-19 DOI: 10.1134/s0016852124700031
A. E. Rybalko, V. A. Shcherbakov, M. Yu. Tokarev, A. A. Kudinov, P. Yu. Belyaev, T. Yu. Repkina, N. E. Zaretskaya, Ya. E. Terekhina, V. V. Ivanova, V. I. Slichenkov

Abstract

The article presents the results of a study of modern geodynamic movements in bottom structures of the White Sea (Baltic Shield). Based on expeditionary work in the White Sea, data were obtained on the formation of the seabed relief and thickness of unconsolidated sediments under the influence of modern seismotectonic events and geodynamic movements, as well as long-term neotectonic processes. It is shown that the Kandalaksha Bay depression is a modern graben developing along faults activated in the Quaternary. Graben development continues to the northwest, where a new Quaternary structure is being formed. Signs of modern geodynamic movements have been identified. The authors demonstrate the role of disjunctive tectonics in the formation of slopes and tectonic structures transverse to the strike of the bay, morphologically represented by relief ridges cutting the Sredny Ludy rise in Kandalaksha Bay. The influence of modern geodynamic processes on the distribution of thicknesses of Quaternary sediments of various genesis and the mosaic distribution of modern bottom sediments has been established. The influence of gravitational processes involved in the formation of underwater landslides, leading to the appearance of abnormally thick layers of the unconsolidated sedimentary cover, has been studied.

摘要 本文介绍了对白海(波罗的海地盾)海底结构中现代地球动力运动的研究结果。根据在白海的考察工作,获得了关于在现代地震构造事件和地球动力运动以及长期新构造过程影响下海底地貌形成和未固结沉积厚度的数据。研究表明,坎达拉克沙湾洼地是沿第四纪活化断层发育的现代地堑。地堑继续向西北方向发展,那里正在形成新的第四纪结构。已发现现代地球动力运动的迹象。作者证明了不连续构造在形成横向于海湾走向的斜坡和构造结构中的作用,在形态上表现为切割坎达拉克沙湾 Sredny Ludy 隆起的地脊。现代地球动力过程对不同成因的第四纪沉积物厚度分布和现代海底沉积物镶嵌分布的影响已经确定。还研究了水下滑坡形成过程中重力作用的影响,这导致了异常厚的未固结沉积覆盖层的出现。
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引用次数: 0
Paleomagnetism of Phanerozoic Strata of the Central Part of the Central Asian Fold Belt 中亚褶皱带中部新生代地层的古地磁学
IF 1.1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-06-19 DOI: 10.1134/s0016852124700018
D. V. Kovalenko, V. V. Yarmolyuk, A. M. Kozlovsky

Abstract

The article summarizes paleomagnetic data for Tuva, Mongolia, and Eastern China, which showed that in the central part of the Central Asian Fold Belt, areas with different paleomagnetic characteristics are distinguished. These are areas located north of the Mongol–Okhotsk mobile belt, the western and eastern parts of Southern Mongolia, and Eastern China. The areas located north of the Mongol–Okhotsk mobile belt were part of the structure of the Siberian continent from the Ordovician and experienced movement similar to the Siberian continent. The regions of the western part of Southern Mongolia have been part of the structure of the Siberian continent since the Late Carboniferous. The geological complexes of the eastern part of Southern Mongolia and blocks of Eastern China in the Middle Paleozoic and Early Mesozoic were located in a latitudinal interval close to the North China block and experienced similar latitudinal movements and rotations. The large difference between the paleolatitudes of coeval strata in western and eastern Mongolia and Eastern China south of the Mongol–Okhotsk mobile belt suggests the existence of a tectonic boundary that separated blocks formed at paleolatitudes along the 107° E meridian, close to Siberia and North China. To the west of the 107° E meridian, the paleolatitudes of the formation of Late Carboniferous–Permian strata are close to the paleolatitudes of Siberia, and east of the meridian, to the paleolatitudes of North China. The width of the Mongol–Okhotsk Ocean in the Late Paleozoic–Early Mesozoic was 30°–40° E (~3000–4000 km). The southern limit of the Mongol–Okhotsk Ocean was segmented and consisted of terranes of various genesis and structure. The closure of segments of the Mongol–Okhotsk Ocean occurred as a result of collision of terranes with the Siberian continent from the Late Carboniferous (in the west) to the Jurassic (in the east).

摘要--文章总结了图瓦、蒙古和中国东部的古地磁数据,结果表明,在中亚褶皱带的中部地区,具有不同的古地磁特征。这些地区分别位于蒙古-奥霍次克移动带以北、南蒙古西部和东部以及中国东部。位于蒙古-奥霍次克移动带以北的地区从奥陶纪起就是西伯利亚大陆结构的一部分,经历了与西伯利亚大陆类似的运动。蒙古南部西部地区从石炭纪晚期开始就是西伯利亚大陆结构的一部分。在中古生代和中生代早期,蒙古南部东部的地质群和中国东部的地块位于靠近华北地块的纬度区间,经历了类似的纬度运动和旋转。蒙古-奥霍次克移动带以南的蒙古西部、东部和华东地区共生地层的古纬度差异很大,这表明在东经107°附近的古纬度上存在着一个构造边界,将靠近西伯利亚和华北的地块分隔开来。在东经 107° 以西,晚石炭-二叠纪地层形成的古地理位置接近西伯利亚的古地理位置,而在东经以东,则接近华北的古地理位置。在晚古生代-中生代早期,蒙古-奥霍次克洋的宽度为东经30°-40°(约3000-4000千米)。蒙古-奥霍次克洋的南缘呈分段状,由不同成因和结构的地层组成。从石炭纪晚期(西部)到侏罗纪(东部),地块与西伯利亚大陆发生碰撞,导致蒙古-奥霍次克洋分段关闭。
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引用次数: 0
Crustal Seismic Anisotropy Beneath the Zagros and Central Iran 扎格罗斯山脉下和伊朗中部的地壳地震各向异性
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2024-04-18 DOI: 10.1134/s0016852124700092
Sh. Mirahmadi, A. Sadidkhouy, Gh. Javan-Doloei, N. Mohammadi

Abstract

The study investigates the variation of shear wave anisotropy among the crustal structure of the Zagros and Central Iran. We used the waveforms of 327 tele-seismic earthquakes with magnitude greater than 5.0 (Mb) at epicentral distances between 30° and 90°, recorded by 22 broadband seismic stations in the study area. The radial and transverse components of the receiver functions in the frequency band from 0.05 to 0.5 Hz were calculated using the earthquakes recorded at each station. Considering t0 as arrival time of the Ps-converted phase on radial receiver functions in the isotropic case, we estimate the effective arrival time for the overlapping phases of the split shear waves as a function of back azimuth. Then we determined the seismic anisotropy parameters of the shear waves (φ, δt). The results show that the average splitting time in the study area varies from 0.24 to 0.65 s, which is a good constraint on the seismic anisotropy compared to the range of crustal seismic anisotropy. Analysis of the fast direction of motion shows that φ changes parallel to the direction of the surface structures and agrees with measurements of the velocity vector GPS that the deformation is rooted in shallower, brittle structures of the crust and active fault zones throughout the environment.

摘要 研究调查了扎格罗斯山脉和伊朗中部地壳结构中剪切波各向异性的变化。我们使用了研究地区 22 个宽带地震台记录的 327 次震级大于 5.0 (Mb)、震中距 30° 至 90° 的远震波形。利用每个台站记录的地震计算了接收函数在 0.05 至 0.5 Hz 频段的径向和横向分量。考虑到 t0 是各向同性情况下 Ps 转换相在径向接收函数上的到达时间,我们估算了作为后方位角函数的分裂剪切波重叠相的有效到达时间。然后,我们确定了剪切波的地震各向异性参数(φ、δt)。结果表明,研究区的平均分裂时间在 0.24 至 0.65 秒之间,与地壳地震各向异性范围相比,对地震各向异性有很好的约束。对快速运动方向的分析表明,φ 的变化平行于地表结构的方向,这与速度矢量 GPS 的测量结果一致,即整个环境中的形变根植于地壳较浅的脆性结构和活动断层带。
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引用次数: 0
Evaluating Tensile Fractures in Rigid Clasts with Very High Aspect Ratio 评估高纵横比刚性碎屑岩的拉伸断裂情况
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2024-04-18 DOI: 10.1134/s0016852124700080
P. Das, S. S. Acharyya, T. K. Mondal, V. Thirukumaran

Abstract

We investigate how a highly elliptical and mechanically rigid clast embedded in an infinite rock mass respond to the far-field stresses. The numerical analysis is carried out on elliptical clasts with aspect ratios ranging from 13.5 to 58.5, oriented at a right angle to the maximum far-field stress. A 2D plane strain model has been adopted to decipher the states of stress inside elliptical clasts. We argue that the tensile stress within the clasts gets enhanced and develops systematic mode-I (tensile) fractures within it as the far-field stress increases. We conclude that the intra-clast tensile stress decreases with increasing clast ellipticity, i.e., tensile fractures develop more easily within clasts with higher aspect ratios (~>20) while a higher far field tensile stress is required to fracture clasts with lower aspect ratios. We also interpret that stress enhancement is independent of the clast area and inter-focii distance of the clast, whilst the aspect ratio of the clast is found to be crucial for the development of tensile fractures within the elliptical clast for a constant material property.

摘要 我们研究了嵌入无限岩体中的高椭圆形机械刚性岩屑对远场应力的响应。数值分析的对象是长宽比从 13.5 到 58.5 的椭圆形岩屑,其方向与最大远场应力成直角。采用二维平面应变模型来解读椭圆形岩屑内部的应力状态。我们认为,随着远场应力的增加,碎屑内部的拉应力会增强,并在其内部形成系统的 I 型(拉伸)断裂。我们的结论是,碎屑内部的拉应力随着碎屑椭圆度的增加而减小,也就是说,在长宽比(~>20)较高的碎屑内部更容易形成拉断裂,而长宽比较低的碎屑则需要较高的远场拉应力才能断裂。我们还解释说,应力增强与岩屑面积和岩屑间距无关,而在材料性质不变的情况下,岩屑的纵横比对椭圆形岩屑内拉伸断裂的发展至关重要。
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引用次数: 0
Structural Reconstruction of the Oligo–Early Miocene Basins of the Eastern Segment of Maghrebian Belt (Northern Tunisia): Influence of Subduction of the Fore-Arc Curvature 马格里布带东段(突尼斯北部)渐新世-早中新世盆地的构造重建:前弧曲俯冲的影响
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2024-04-18 DOI: 10.1134/s0016852124700055
R. Azizi, N. Mahmoudi, S. Gaieb, H. Mnasri, Y. Houla, Ch. Mezni

Abstract

Based on the field observations and tectono-sedimentary analysis, we suggest reconstruction of the geological evolution from case study of Northern Tunisia since the Eocene age. The reconstruction of the structural architecture of this region can be aided by knowing the spatiotemporal occurrence and the deformation of the Oligo‒Early Miocene deposits. In the research area, two depositional basin types that coexisted but in different tectonic settings were seen in the reconstruction of Oligo‒Early Miocene successions. In Northern Tunisia, the Late Eocene shortening episode led to a thin-skinned deformation that produced irregular basement topography. During the Oligo‒Early Miocene subduction process, the earliest lithofacies of the Maghrebian Numidian flysch deposited in deep marine offshore environment. Synchronously in the onshore, the second lithofacies of Fortuna were deposited in NW-trending extensional structures after a rifting episode that characterized north-eastern Tunisia (ante-nappes). During the Middle Miocene, the curving fore-arc of subduction between Africa and the Mesomediterranean Microplate dominated northern Tunisia. As a result, the Numidian basin was raised, resulting in thrust sheets in northwestern part of Tunisia, while the extensional structures supporting the Fortuna succession were closed and created push-up structures following transpressional deformation along the NW‒SE boundary faults. Continental collision has occurred in northern Tunisia since the Late Miocene, resulting in shortening structures, some elevated areas, and sedimentary gaps encompassing a substantial portion of the study area.

摘要根据实地观察和构造沉积分析,我们建议通过对突尼斯北部的案例研究重建自始新世以来的地质演变。了解渐新世-早中新世沉积物的时空分布和变形情况有助于重建该地区的构造体系。在该研究地区,在重建渐新世-早中新世的演替过程中发现了两种共存但构造环境不同的沉积盆地类型。在突尼斯北部,晚始新世的缩短导致了薄层变形,产生了不规则的基底地形。在渐新世-早中新世的俯冲过程中,马格里布努米底亚飞沙的最早岩性沉积在深海近海环境中。与此同时,在突尼斯东北部(前中新世)发生断裂之后,Fortuna 的第二批岩性沉积在西北走向的伸展构造中。在中新世时期,非洲与中地中海微板块之间俯冲的弯曲前弧主导了突尼斯北部。因此,Numidian 盆地隆起,在突尼斯西北部形成了推力片,而支撑 Fortuna 演替的伸展构造则被封闭,并在沿 NW-SE 边界断层发生转位变形后形成了推升构造。自晚中新世以来,突尼斯北部发生了大陆碰撞,导致结构缩短,一些地区隆起,沉积间隙覆盖了研究区域的很大一部分。
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引用次数: 0
Transpressive Tectonics Evidence in the Epicentral Area of the Modern Earthquake in Constantine Area of Algerian Eastern Tell Atlas: New Insights from Rhumel Valley 阿尔及利亚东泰勒阿特拉斯地区君士坦丁现代地震震中区的透射构造证据:来自鲁梅尔山谷的新见解
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2024-04-18 DOI: 10.1134/s0016852124700067
S. Aourari, D. Machane, M. Guemache, H. Haddoum, A. Benhamouche, H. Moulouel, S. Sadrati, N. Sidi Said, D. Ait Benamar

Abstract

The neotectonic processes are crucial for identification of active faults in a seismic unstable area. The Aїn Smara active fault runs along the Middle Rhumel Valley located in Constantine area of Algerian Eastern Tell Atlas mountain chain and it emerges in the south‒western part of the epicentral zone of the earthquake occurred on October 27, 1985 (Mw = 5.8) within a corridor displaying morphological features and deformed Pliocene‒Quaternary layers, which are the consequence of transpressive tectonic regime. In our study the morpho-tectonic and structural research supported by the fieldwork, was performed. The thick fault gouge indicating simple shear deformation, fault breccias and minor faults affecting the Pliocene limestone and Quaternary alluvial terraces, were found. The active fault splits into northern and southern segments. The northern segment corresponds to the El Aria Fault that ruptured during the earthquake in 1985 and the southern segment with the studied Aĭn Smara Fault. Our research showed the significant extent of the active fault and including its parameters for improved seismic hazard assessment of the Constantine area.

摘要 新构造过程对于识别地震不稳定地区的活动断层至关重要。艾因斯马拉活动断层沿着位于阿尔及利亚东泰勒阿特拉斯山脉康斯坦丁地区的中鲁梅尔山谷运行,它位于 1985 年 10 月 27 日发生的地震(Mw = 5.8)震中区的西南部,在一条走廊内显示出形态特征和上新世-第四纪地层变形,这是转位构造机制的结果。在我们的研究中,在实地考察的支持下进行了形态构造和结构研究。我们发现了厚厚的断层冲沟,表明了简单的剪切变形、断层破碎带和影响上新世石灰岩和第四纪冲积阶地的小断层。活动断层分为南北两段。北段与 1985 年地震中断裂的 El Aria 断层相对应,南段与研究中的 Aĭn Smara 断层相对应。我们的研究显示了活动断层的重要范围,并将其参数纳入其中,以改进君士坦丁地区的地震灾害评估。
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引用次数: 0
Strain Analysis and Microstructural Study of Hamadat Core Complex, Northwestern Arabian Shield, Saudi Arabia 沙特阿拉伯西北阿拉伯地盾哈马达特岩芯群的应变分析和微结构研究
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2024-04-18 DOI: 10.1134/s0016852124700079
M. H. Al-Hashim, O. M. K. Kassem

Abstract

The present work illustrates the structural setting in the Hamadat core complex, which located in the Midyan terrane. It is essential to understand deformational processes and products at different scales, which depend on the calculation of finite strain. To assess the tectonic development and structures in the Hamadat core complex, we use field investigation, finite strain analysis and microstructural examination. The Hamadat core complex employed the Rf/φ and Fry techniques for feldspar and mafic grains with 24 collected samples for gneisses, metavolcano-sedimentary rocks from both the Zaam and Baydah groups, deformed granodiorite for Jar-Salajah intrusion and Qazzaz granite. According to finite-strain data, the various rock units have moderate to high degree of deformation, and the axial ratios for XZ section vary from 1.80 to 4.50 for the Rf/φ technique and from 2.10 to 7.40 for the Fry technique. It concluded that the shortening axes display the subvertical related to the subhorizontal foliation. The strain data have the same main-phase foliation and similar deformation behavior. Finite strain acquired through high pressure metamorphism in this instance suggested that the contacts of nappe developed through the buildup of ductile strains. Also, during thrusting and intrusions throughout the deformation process, a building of brittle to ductile deformation was mostly caused by pure shearing in the study area.

摘要 本研究说明了位于米迪亚地层的哈马达特岩芯复合体的结构环境。了解不同尺度的变形过程和产物至关重要,而这取决于有限应变的计算。为了评估哈马达特岩芯群的构造发展和结构,我们采用了实地考察、有限应变分析和微结构检查等方法。哈马达特岩芯群采用了长石和黑云母晶粒的 Rf/φ 和 Fry 技术,采集了 24 个样品,包括片麻岩、Zaam 组和 Baydah 组的变火山沉积岩、Jar-Salajah 侵入体的变形花岗闪长岩和 Qazzaz 花岗岩。根据有限应变数据,各种岩石单元具有中度到高度变形,XZ 断面的轴向比(Rf/φ 技术)从 1.80 到 4.50 不等,而 Fry 技术则从 2.10 到 7.40 不等。其结论是,缩短轴显示出与亚水平褶皱相关的亚垂直褶皱。应变数据具有相同的主相褶皱和相似的变形行为。在这种情况下,通过高压变质作用获得的有限应变表明,岩层的接触是通过韧性应变的积累而形成的。此外,在整个变形过程中的推力和侵入过程中,脆性变形到韧性变形的建立主要是由研究区域的纯剪切引起的。
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引用次数: 0
The Pre-Quaternary Evolution of the Eurasia Basin: The Results of Interpretation of Seismic Profile ARC1407A 欧亚大陆盆地的前第四纪演化:ARC1407A 地震剖面的解释结果
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2024-03-14 DOI: 10.1134/s0016852123060080
A. V. Zayonchek, S. Yu. Sokolov, A. V. Soloviev

Abstract

This paper presents the results of a study of the pre-Quaternary tectonics and stratigraphy of the Eurasia Basin (EB) according to the interpretation of the ARC1407A seismic profile and calculations of the theoretical positions of linear magnetic anomalies. The sedimentary sequences are recognized in seismic profiles and their stratigraphic position is similar to that of sedimentary sequences in the western parts of the Nansen and Amundsen basins. The age indexation of sedimentary sequences corresponds to the ACEX drilling results and the main evolution stages of the EB. No previously recognized reference horizon with the age of ~34 Ma, which is related to the termination of spreading in the western part of North Atlantic and amalgamation of the Greenland and North American plates, is recognized, as is supported by our studies in the western parts of the EB. In the western part of the Nansen Basin we identified a reference horizon with the age of 38 Ma for the first time, which was previously traced in the western part of the Amundsen Basin, whose formation is related to the evolution stage of the Eurekan Orogen. A reference horizon with the age of ~26 Ma, which has been traced in the western part of the Amundsen Basin before, is also distinguished in the western part of the Nansen Basin within ARC1407A. This geological boundary is related to the beginning of unstable spreading in the western segment of the EB between the Yermak Plateau and Morris Jessup Rise (Plateau). The end of a long stratigraphic hiatus between 44.4 and 18.2 Ma in the section of ACEX boreholes is clearly correlated with the formation of a sedimentary sequence of ~19.6‒18.3 Ma, which is the age of the beginning of the formation of a deep-water gateway between the North Atlantic and Eurasian sedimentary basins. This event coincides with the main reconstruction stage of movements of the Eurasia and North America plates, which led to a change in the direction of migration of momentary opening poles from the NNW to SSE. It is suggested that the thick sedimentary sequences in the Nansen Basin and the rift valley of the Gakkel Ridge that are observed in seismic section ARC1407A include Late Pliocene–Quaternary (<2.7 Ma) glaciomarine rocks, which compose a significant volume of sediments in the eastern part of the EB and the Gakkel Ridge.

摘要 本文介绍了根据 ARC1407A 地震剖面解释和线性磁异常理论位置计算对欧亚盆地(EB)前第四纪构造和地层研究的结果。地震剖面识别了沉积序列,其地层位置与南森盆地和阿蒙森盆地西部的沉积序列相似。沉积序列的年龄指数与 ACEX 钻井结果和 EB 的主要演化阶段相符。我们在 EB 西部地区的研究证实了这一点,目前尚未发现与北大西洋西部扩张终止以及格陵兰板块和北美板块合并有关的年龄为约 34 Ma 的参考层。在南森盆地西部,我们首次发现了一个年龄为 38 Ma 的参照层,此前我们曾在阿蒙森盆地西部追踪到这一参照层,其形成与厄勒干造山运动的演化阶段有关。在 ARC1407A 内的南森盆地西部也发现了一个年龄约为 26 Ma 的参照层,该参照层曾在阿蒙森盆地西部被追踪到。这一地质界线与叶尔马克高原和莫里斯-杰瑟普隆起(高原)之间的 EB 西段不稳定扩张的开始有关。在 ACEX 钻孔剖面中,44.4-18.2Ma 之间漫长地层间断的结束与 ~19.6-18.3 Ma 沉积序列的形成明显相关,而这正是北大西洋与欧亚沉积盆地之间深水门户开始形成的年代。这一事件与欧亚板块和北美板块运动的主要重建阶段相吻合,这导致了瞬时开口极的迁移方向从西北偏北转向东南偏东。ARC1407A 地震剖面中观察到的南森盆地和加克尔海脊裂谷的厚沉积层序包括晚更新世-第四纪(2.7Ma)冰川岩,这些冰川岩构成了 EB 东部和加克尔海脊的大量沉积物。
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Geotectonics
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