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Spatial distribution features of sequence types of moderate and strong earthquake in Chinese mainland

机译:中国大陆中强烈地震序列类型的空间分布特征

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摘要

Based on 294 earthquake sequences with magnitude greater than or equal to 5.0 occurred in Chinese mainland since 1970, the spatial distribution features of sequence types have been studied. In southwestern China, it takes mainshock-aftershock sequence type (MAT) as the major in Chuan-Dian rhombic block and concerned Xianshuihe-Anninghe-Xiaojiang seismic belt, as well as in Jinshajiang-Honghe seismic belt. Multiple mainshock type (MMT) mainly distributes in western Yunnan, and Longlin and Lancang areas in Tengchong-Baoshan block in west of Nujiang-Lancangjiang fault zone. A few isolated earthquake type (IET) mainly occurred in northwestern Sichuan and there is no IET occurred in Yunnan region. In northwestern China, it takes mainshock-aftershock sequence type (MAT) as the major in west segment of South Tianshan in Xinjiang region. Some MMT also occurred in this area in the intersection of Kalpin block and the Puchang fault zone. It takes IET as the major in middle Tianshan in Xinjiang. Along the Qilianshan seismic belt, most of sequences are MAT. In Qinghai region, it takes MAT as the major, but the regional feature of the spatial distribution of sequence types is not very clear. In North China, it takes MAT as the major in Yinshan-Yanshan-Bohai seismic belt, north edge of North China, and in Hebei plain seismic belt, as well as in sub-plate of lower river area of Yangtze River. In intersection of north segment of Shanxi seismic belt and the NW-trending Yinshan-Yanshan-Bohai seismic belt, there are several moderate or strong MMT with magnitude from 5.0 to 6.0 occurred. In south of North China around the latitude line of 35°N, it takes IET as the major. The spatial distribution of sequence types is relevant to the patterns of tectonic movements. MAT is mostly produced by the ruptures of locked units or asperities or the neonatal separating segments inside the fault zones. MMT is generally relevant to the conjugate structures or intersection of many tectonic settings. Further extension of simple fault often produces IET. Spatial distribution of sequence types is also correlative to the regional and deep environment of crustal medium to some extent. MAT mainly distributes in high velocity area in upper crust or in the transition zone between high velocity area and low velocity area, MMT mostly occurred in the low velocity area in upper crust.
机译:根据1970年以来中国大陆发生的294个大于或等于5.0的地震序列,对序列类型的空间分布特征进行了研究。在西南地区,川滇菱形块体以主震-余震序列类型(MAT)为主要震源,与咸水河-安宁河-小江地震带以及金沙江-红河地震带有关。多重主震型(MMT)主要分布在云南西部,怒江-澜沧江断裂带以西的腾冲-宝山地块的龙林和澜沧地区。少数孤立地震类型(IET)主要发生在四川西北部,云南地区没有发生IET。在中国西北地区,它以主震-余震序列类型(MAT)为主要区域,在新疆地区南天山西段。在卡尔平地块与普厂断裂带相交处的该区域也发生了一些MMT。它以IET作为新疆天山中段的专业。沿祁连山地震带,大部分序列是MAT。在青海地区,以MAT为主要内容,但序列类型空间分布的区域特征不是很清楚。在华北地区,以MAT为主,在银山-燕山-渤海地震带,华北北部边缘,河北平原地震带以及长江下游子板块中。在山西地震带北段与西北走向的阴山—燕山—渤海地震带的交汇处,出现了数个中等或强的MMT,震级范围为5.0〜6.0。在华北以35°N纬线为中心,以IET为主要。层序类型的空间分布与构造运动的模式有关。 MAT的产生主要是由断层区域内锁定单元或凹凸的破裂或新生儿分离段引起的。 MMT通常与共轭结构或许多构造背景的交集有关。简单故障的进一步扩展通常会产生IET。序列类型的空间分布在某种程度上也与地壳介质的区域和深层环境有关。 MAT主要分布在上地壳的高速区或高速区与低速区之间的过渡带,MMT主要发生在上地壳的低速区。

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