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首页> 外文期刊>International Geology Review >Late Mesozoic rift evolution and crustal extension in the central Songliao Basin, northeastern China: constraints from cross-section restoration and implications for lithospheric thinning
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Late Mesozoic rift evolution and crustal extension in the central Songliao Basin, northeastern China: constraints from cross-section restoration and implications for lithospheric thinning

机译:中国东北松辽盆地中部晚中生代裂谷演化和地壳扩展:剖面恢复的约束及其对岩石圈变薄的影响

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摘要

The Songliao Basin, the largest oil-producing basin in China, was the centre of late Mesozoic rifting and lithospheric thinning in northeastern China. However, the rifts are still poorly revealed due to a thick cover of subsidence successions. By structural interpretation and sequential restoration of cross-sections based on new 2D seismic data and well data, this study presents the structural style, basin evolution, and horizontal crustal extension of the central Songliao Basin. We have developed a novel method to retrieve the regional extension principal strains. The results enable an assignment of rifting into two episodes. The earlier episode (ca. 157-130Â Ma) was dominated by distributed faulting of numerous planar normal faults trending NNE-SSW, NNW-SSE, or near NS, probably reflecting pre-existing basement fabrics; in contrast, the later episode (ca. 130-102Â Ma) was controlled by localized extension along several major listric faults. Horizontal crustal extension during rifting is estimated to have been 11-28Â km (10.6%-25.5%), with the long-term average rate varying from 0.20 to 0.51Â mm yr-1. Regional horizontal strains show a gradual evolution from biaxial extension at the beginning of rifting to WNW-ESE uniaxial stretching during the later rifting episode. Brittle crustal extension is interpreted to have been associated with vertical strain due to tectonic stretching, which is estimated to have contributed more in thinning the lower crust than the mantle lithosphere. Accordingly, a two-episode dynamic model is proposed to explain rifting in the Songliao Basin. We suggest that the earlier event was dominated by delamination of the thickened continental lithosphere, whereas the later event was probably controlled by regional crustal detachment due to slab subduction and stagnancy of the Izanagi lithospheric plate.View full textDownload full textKeywordsSongliao Basin, cross-section restoration, rift, extensional tectonics, lithospheric thinningRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/00206814.2010.511900
机译:松辽盆地是中国最大的产油盆地,是中国东北中生代晚期裂谷和岩石圈变薄的中心。但是,由于沉陷演替的覆盖很深,因此裂痕仍然显示得很差。通过基于新的2D地震数据和井数据的结构解释和剖面的顺序恢复,本研究提出了松辽盆地中部的构造样式,盆地演化和水平地壳扩展。我们已经开发出一种新颖的方法来检索区域扩展主要菌株。结果可以将裂痕分成两集。较早的时期(大约157-130 Ma)主要由大量的平面正断层分布的断层所主导,这些断层趋向于NNE-SSW,NNW-SSE或靠近NS的地方,这可能反映了已有的基底构造。相反,后期(大约130-102 Ma)是由沿几个主要李斯特断裂的局部扩展控制的。在裂谷过程中,水平地壳扩展估计为11-28 km(10.6%-25.5%),长期平均速率从0.20到0.51 mm yr -1 不等。区域水平应变显示了从裂谷开始时的双轴延伸到后来的裂谷事件中的WNW-ESE单轴拉伸的逐渐演变。脆性的地壳伸展被认为是由于构造伸展引起的垂直应变,与地幔岩石圈相比,地壳伸展变薄的作用更大。因此,提出了两段动力学模型来解释松辽盆地的裂谷作用。我们认为较早的事件以增厚的大陆岩石圈的剥脱为主导,而较晚的事件可能是由于伊萨纳吉岩石圈板块的俯冲和停滞而受到区域地壳脱离的控制。查看全文下载全文关键词,裂谷,伸展构造学,岩石圈变薄ra-4dff56cd6bb1830b“};添加到候选列表链接永久链接http://dx.doi.org/10.1080/00206814.2010.511900

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