牛首山-罗山断裂带的变形特征及其构造意义
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摘要
牛首山-罗山断裂带是青藏高原东北缘最外侧的一条断裂带,其空间分布、深部结构、运动学特征以及变形机制对研究青藏高原东北角弧形断裂系的形成与演化具有重要意义。文中通过对横穿牛首山-罗山的4条地震反射剖面的解释及断裂带部分地区大比例尺的构造地质填图,发现牛首山-罗山断裂带具有不连续性与分段性。断裂带南段罗山断裂以正花状构造为特征,显示断裂具有右旋走滑性质;中段牛首山东麓断裂可能并不存在,该区以强烈的褶皱变形为特征;北段三关口断裂则以左旋走滑为特征。牛首山-罗山断裂带的这种不连续性和分段性反映了断裂带的不同构造部位在青藏高原向NE方向扩展过程中具有不同的变形样式。
As the outermost fault zone in the northeastern margin of the Tibetan plateau,the deep structures,distribution,movement feature and deformational mechanism of the Niushoushan-Luoshan Fault zone are crucial to understand the formation and evolution of the arcuate fault zones in the northeast corner of the Tibetan plateau. In this paper,we analyze four seismic reflection sections across the Niushoushan-Luoshan Fault zone and map in detail the area within the fault zone. These data indicate that the Niushoushan-Luoshan Fault zone is a discrete fault zone. The fault zone can be subdivided into three parts: the south part,i. e. the Luoshan Fault,is characterized by positive flower structure,shown as remarkable right lateral strike-slip; in the middle segment,that is,the Niushoushan Fault,no active fault exists on the east flank of the Niushoushan,and this region is dominated by intensive folding; the north part,the Sanguankou Fault,is a left-lateral strike-slip fault. The discontinuity and segmentation feature of the Niushoushan-Luoshan Fault zone suggest different deformational styles in different locations of the fault zone associated with the process of northeastward propagation of the Tibetan plateau.
As the outermost fault zone in the northeastern margin of the Tibetan plateau,the deep structures,distribution,movement feature and deformational mechanism of the Niushoushan-Luoshan Fault zone are crucial to understand the formation and evolution of the arcuate fault zones in the northeast corner of the Tibetan plateau. In this paper,we analyze four seismic reflection sections across the Niushoushan-Luoshan Fault zone and map in detail the area within the fault zone. These data indicate that the Niushoushan-Luoshan Fault zone is a discrete fault zone. The fault zone can be subdivided into three parts: the south part,i. e. the Luoshan Fault,is characterized by positive flower structure,shown as remarkable right lateral strike-slip; in the middle segment,that is,the Niushoushan Fault,no active fault exists on the east flank of the Niushoushan,and this region is dominated by intensive folding; the north part,the Sanguankou Fault,is a left-lateral strike-slip fault. The discontinuity and segmentation feature of the Niushoushan-Luoshan Fault zone suggest different deformational styles in different locations of the fault zone associated with the process of northeastward propagation of the Tibetan plateau.
引文
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王伟涛,张培震,张广良,等.2010.青藏高原东北缘寺口子盆地新生代沉积演化及其构造意义[J].地质科学,45(2):440—452.WANG Wei-tao,ZHANG Pei-zhen,ZHANG Guang-liang,et al.2010.Cenozoic sedimentary evolution of the SikouziBasin on the northeastern margin of the Qinghai-Tibetan plateau and its tectonic significance[J].Chinese Journalof Geology,45(2):440—452(in Chinese).
王志才,张培震,张广良,等.2006.西秦岭北缘构造带的新生代构造活动:兼论对青藏高原东北缘形成过程的指示意义[J].地学前缘,13(4):119—135.WANG Zhi-cai,ZHANG Pei-zhen,ZHANG Guang-liang,et al.2006.Tertiary tectonic activities of the north frontal faultzone of the west Qinling Mountains:Implications for the growth of the northeastern margin of the Qinghai-Tibetanplateau[J].Earth Science Frontiers,13(4):119—135(in Chinese).
徐锡伟,Tapponnier P,Van Der Woerd J,等.2003.阿尔金断裂带晚第四纪左旋走滑速率及其构造运动转换模式讨论[J].中国科学(D),33(10):967—974.XU Xi-wei,Tapponnier P,Van Der Woerd J,et al.2003.Pattern of latest tectonic motion and its dynamics for activeblocks in Sichuan-Yunnan region,China[J].Science in China(Ser D),33(10):967—974(in Chinese).
袁道阳,张培震,刘百篪,等.2004.青藏高原东北缘晚第四纪活动构造的几何图像与构造转换[J].地质学报,78(2):270—278.YUAN Dao-yang,ZHANG Pei-zhen,LIU Bai-chi,et al.2004.Geometrical imagery and tectonic transformation of lateQuaternary active tectonics in northeastern margin of Qinghai-Xizang Plateau[J].Acta Geologica Sinica,78(2):270—278(in Chinese).
袁道阳,张培震,雷中生,等.2005.青海拉脊山断裂带新活动特征的初步研究[J].中国地震,21(1):93—102.YUAN Dao-yang,ZHANG Pei-zhen,LEI Zhong-sheng,et al.2005.A preliminary study on the new activity features ofthe Lajishan Mountain Fault zone in Qinghai Province[J].Earthquake Research in China,21(1):93—102(inChinese).
袁道阳,张培震,方小敏,等.2007.青藏高原东北缘临夏盆地晚新生代构造变形及过程[J].地学前缘,14(1):243—250.YUAN Dao-yang,ZHANG Pei-zhen,FANG Xiao-min,et al.2007.Late Cenozoic tectonic deformation of the LinxiaBasin,northeastern margin of the Qinghai-Tibet Plateau[J].Earth Science Frontiers,14(1):243—250(inChinese).
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