伊豆−博宁−马里亚纳岛弧地壳厚度分布及其对岩浆活动的指示     

白永良  杨慧良  张迪娅  容伊霖  董冬冬  吴时国 《海洋地质与第四纪地质》2021,(1):158-165

数值模拟研究认为洋底高原/洋脊俯冲和弧后扩张能够有效影响俯冲带岩浆活动和岛弧地壳增生。本文以伊豆?博宁?马里亚纳(IBM)俯冲带为实例,论证该结论的有效性。以卫星测高反演重力异常为基础,通过构建地球不同圈层密度模型,反演得到IBM俯冲带莫霍面埋深。本文的莫霍面埋深反演结果与地震解释结果具有一致的分布趋势。结合开源水深和沉积层厚度数据,给出了IBM俯冲带地壳厚度分布。IBM岛弧地壳体积沿走向的分布特征表明:①小笠原洋底高原和相对较小规模达顿洋脊的俯冲,都能够使得相应位置的岛弧变窄、地壳变厚、体积增大;②马里亚纳海槽扩张显著降低了岛弧地壳体积的增生量。  相似文献   

A complete series of C31–C34 25-norbenzohopanes in the Devonian and Jurassic bitumen sands,NW Sichuan Basin     

《Organic Geochemistry》2012

A complete series of C₃₂–C₃₅ benzohopanes and corresponding C₃₁–C₃₄ 25-norbenzohopanes were tentatively identified in Devonian and Jurassic bitumen sands from the northwestern Sichuan Basin in southwestern China. Although other origins cannot be excluded, the relative distributions of C₃₂–C₃₅ benzohopanes and C₃₁–C₃₄ 25-norbenzohopanes, along with other biomarker parameters, suggest that the 25-norbenzohopanes formed by demethylation of the corresponding benzohopanes.  相似文献   

Geological controls on focused fluid flow through the gas hydrate stability zone on the southern Hikurangi Margin of New Zealand,evidenced from multi-channel seismic data     

《Marine and Petroleum Geology》2012,29(10):1915-1931

Highly concentrated gas hydrate deposits are likely to be associated with geological features that promote increased fluid flux through the gas hydrate stability zone (GHSZ). We conduct conventional seismic processing techniques and full-waveform inversion methods on a multi-channel seismic line that was acquired over a 125 km transect of the southern Hikurangi Margin off the eastern coast of New Zealand’s North Island. Initial processing, employed with an emphasis on preservation of true amplitude information, was used to identify three sites where structures and stratal fabrics likely encourage focused fluid flow into and through the GHSZ. At two of the sites, Western Porangahau Trough and Eastern Porangahau Ridge, sub-vertical blanking zones occur in regions of intensely deformed sedimentary layering. It is interpreted that increased fluid flow occurs in these regions and that fluids may dissipate upwards and away from the deformed zone along layers that trend towards the seafloor. At Eastern Porangahau Ridge we also observe a coherent bottom simulating reflection (BSR) that increases markedly in intensity with proximity to the centre of the anticlinal ridge. 1D full-waveform inversions conducted at eight points along the BSR reveal much more pronounced low-velocity zones near the centre of the ridge, indicating a local increase in the flux of gas-charged fluids into the anticline. At another anticline, Western Porangahau Ridge, a dipping high-amplitude feature extends from the BSR upwards towards the seafloor within the regional GHSZ. 1D full-waveform inversions at this site reveal that the dipping feature is characterised by a high-velocity zone overlying a low-velocity zone, which we interpret as gas hydrates overlying free gas. These results support a previous interpretation that this high-amplitude feature represents a local “up-warping” of the base of hydrate stability in response to advective heat flow from upward migrating fluids. These three sites provide examples of geological frameworks that encourage prolific localised fluid flow into the hydrate system where it is likely that gas-charged fluids are converting to highly concentrated hydrate deposits.  相似文献   

基于多特征的Gaofen-1海冰影像监督分割     

陈科铭  郭梦  江一明 《测绘与空间地理信息》2021,44(1):122-125

冬季沿海地区的海冰检测工作对该地区居民的生产生活具有重要的指导意义,同时可以根据海冰变化检测气候变暖情况。海冰影像分割是海冰检测的基础。在众多海冰影像数据源中,Gaofen-1海冰影像因其丰富的光谱特征、较高的空间分辨率、简单的数据结构,在变化监测中具有重要应用价值。本文提出了一种基于红绿蓝3个光谱通道的灰度共生矩阵,提取遥感影像的纹理特征和光谱特征构成多特征的Gaofen-1海冰影像监督分割方法。以Gaofen-1合成的模拟海冰影像和某海湾地区真实Gaofen-1海冰影像进行分割实验,实验结果很好地证明了算法的可行性和可靠性。  相似文献   

基于GAMIT数据解算的CORS站点稳定性分析研究     

符平伟  黄克城 《测绘与空间地理信息》2021,44(1):126-129,133

以2013年建成使用的三亚市连续运行参考站综合服务系统(SYCORS)的五个参考站点为例,通过采集2014—2015年多期观测数据,并结合建站数据成果进行对比,研究利用GAMIT软件进行CORS站点的稳定性监测分析。研究结果表明:该研究区域的CORS系统参考站网间稳定性较好,同时证明了利用GAMIT软件进行CORS站点稳定性监测分析的方法可行,可在CORS系统站点稳定性常态化更新维护等工作中运用。  相似文献   

Failure of landslide stabilization measures: The Sidi Rached viaduct case (Constantine,Algeria)     

Mehdi A. Guemache  Jean-Luc Chatelain  Djamel Machane  Sihem Benahmed  Leila Djadia 《Journal of African Earth Sciences》2011,59(4-5):349-358

The goal of this paper is to document causes of the failure of stabilization measures undertaken for stabilizing a complex landslide threatening the Sidi Rached viaduct in Constantine, Algeria. Since the first instabilities, documented in 1910 during its construction, significant disturbances have been regularly observed on its eastern part and reinforcements carried out were only temporarily effective. Observed disturbances are inherently related to the fact that the eastern abutment and the three subsequent piers are built on unstable Maastrichtian marls whereas the remainder of the viaduct rests on stable Turonian limestone. The five main factors controlling the activation of the failure process are reviewed: (1) geomorphology, (2) geology, (3) human activities, (4) climate, and (5) seismicity. Data interpretation of two inclinometer surveys carried out close to the eastern abutment shows that the unstable mass moves westward, towards the Rhumel gorges. The main slip surface is located in the Maastrichtian schistose marl, at a depth ranging from about 8 m (west) to about 30 m (east). This translational slide is associated with a settling phenomenon due to the petrophysical properties of the unstable marl.  相似文献   

In Situ Measurements of the Raman Shifts for ν1 Symmetric Stretching Band of CH4 Between -180 and 350 oC with Densities up to 0.45 g/cm3 in Optical Cells with Fused Silica Windows     

SHANG Linbo  I-Ming CHOU  HU Ruizhong  BI Xianwu 《地质学报》2013,87(Z1):333-334

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The Perspective of Deep-sea Science Research and the Establishment of Modern Hydrothermal Laboratories in China     

I-Ming CHOU 《地质学报》2013,87(Z1):3-4

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The tectonic evolution of the Qiongdongnan Basin in the northern margin of the South China Sea     

《Journal of Asian Earth Sciences》2013

Qiongdongnan Basin is a Cenozoic rift basin located on the northern passive continental margin of the South China Sea. Due to a lack of geologic observations, its evolution was not clear in the past. However, recently acquired 2-D seismic reflection data provide an opportunity to investigate its tectonic evolution. It shows that the Qiongdongnan Basin comprises a main rift zone which is 50–100 km wide and more than 400 km long. The main rift zone is arcuate in map view and its orientation changes from ENE–WSW in the west to nearly E–W in the east. It can be divided into three major segments. The generally linear fault trace shown by many border faults in map view implies that the eastern and middle segments were controlled by faults reactivated from NE to ENE trending and nearly E–W trending pre-existing fabrics, respectively. The western segment was controlled by a left-lateral strike-slip fault. The fault patterns shown by the central and eastern segments indicate that the extension direction for the opening of the rift basin was dominantly NW–SE. A semi-quantitative analysis of the fault cut-offs identifies three stages of rifting evolution: (1) 40.4–33.9 Ma, sparsely distributed NE-trending faults formed mainly in the western and the central part of the study area; (2) 33.9–28.4 Ma, the main rift zone formed and the area influenced by faulting was extended into the eastern part of the study area and (3) 28.4–20.4 Ma, the subsidence area was further enlarged but mainly extended into the flanking area of the main rift zone. In addition, Estimates of extensional strain along NW–SE-trending seismic profiles, which cross the main rift zone, vary between 15 and 39 km, which are generally comparable to the sinistral displacement on the Red River Fault Zone offshore, implying that this fault zone, in terms of sinistral motion, terminated at a location near the southern end of the Yinggehai Basin. Finally, these observations let us to favour a hybrid model for the opening of the South China Sea and probably the Qiongdongnan Basin.  相似文献   

Different expressions of rifting on the South China Sea margins     

《Marine and Petroleum Geology》2014

Rifting of continental margins is generally diachronous along the zones where continents break due to various factors including the boundary conditions which trigger the extensional forces, but also the internal physical boundaries which are inherent to the composition and thus the geological history of the continental margin. Being opened quite recently in the Tertiary in a scissor-shape manner, the South China Sea (SCS) offers an image of the rifting structures which varies along strike the basin margins. The SCS has a long history of extension, which dates back from the Late Cretaceous, and allows us to observe an early stretching on the northern margin onshore and offshore South China, with large low angle faults which detach the Mesozoic sediments either over Triassic to Early Cretaceous granites, or along the short limbs of broad folds affecting Palaeozoic to Early Cretaceous series. These early faults create narrow troughs filled with coarse polygenic conglomerate grading upward to coarse sandstone. Because these low-angle faults reactivate older trends, they vary in geometry according to the direction of the folds or the granite boundaries. A later set of faults, characterized by generally E–W low and high angle normal faults was dominant during the Eocene. Associated half-graben basement deepened as the basins were filling with continental or very shallow marine sediments. This subsequent direction is well expressed both in the north and the SW of the South China Sea and often reactivated earlier detachments. At places, the intersection of these two fault sets resulting in extreme stretching with crustal boudinage and mantle exhumation such as in the Phu Khanh Basin East of the Vietnam fault. A third direction of faults, which rarely reactivates the detachments is NE–SW and well developed near the oceanic crust in the southern and southwestern part of the basin. This direction which intersects the previous ones was active although sea floor spreading was largely developed in the northern part, and ended by the Late Miocene after the onset of the regional Mid Miocene unconformity known as MMU and dated around 15.5 Ma. Latest Miocene is marked by a regional basement drop and localized normal faults on the shelf closer to the coast. The SE margin of the South China Sea does not show the extensional features as well as the Northern margin. Detachments are common in the Dangerous Grounds and Reed Bank area and may occasionally lead to mantle exhumation. The sedimentary environment on the extended crust remained shallow all along the rifting and a large part of the spreading until the Late Miocene, when it suddenly deepened. This period also corresponds to the cessation of the shortening of the NW Borneo wedge in Palawan, Sabah, and Sarawak. We correlate the variation of margin structure and composition of the margin; mainly the occurrence of granitic batholiths and Mesozoic broad folds, with the location of the detachments and major normal faults which condition the style of rifting, the crustal boudinage and therefore the crustal thickness.  相似文献