地震地质
地震地質
지진지질
SEISMOLOGY AND GEOLOGY
2002年
1期
14-26
,共13页
何宏林%池田安隆%宋方敏%董兴权
何宏林%池田安隆%宋方敏%董興權
하굉림%지전안륭%송방민%동흥권
活动断层%滑动速率%小江断裂带%青藏高原东南
活動斷層%滑動速率%小江斷裂帶%青藏高原東南
활동단층%활동속솔%소강단렬대%청장고원동남
Active fault%Slip rate%Xiaojiang fault%Southeastern Tibet
位于中国西南的小江(Xiaojiang)断裂带作为康定(Kangding)断裂带的南段,在青藏块体向SE方向挤出的过程中起着重要的作用.根据断错地貌以及这些断错地貌14C年代或热释光年代,推算了小江断裂带第四纪晚期的左旋走滑速率.小江断裂带可以分为3段,其中段由平行的两条断层组成.西支断层和东支断层的左旋走滑速率分别为7.0~9.0mm/yr和6.0~7.5mm/yr.简单相加,就可以推算出小江(Xiaojiang)断裂带总的左旋走滑速率为13.0~16.5mm/yr,与康定断裂带北段的鲜水河(Xianshuihe)断层的走滑速率大致相当,约等于康定(Kangding)断裂带中段的安宁河(Anninghe)断层及则木河(Zemuhe)断层的两倍.这个结果可能暗示了在康定断裂带中段,可能存在着其他断层以解消另外一半的滑动速率.最有可能的断层是位于康定断裂带中段以东几十公里的普雄河-布拖(Puxionghe-Butuo)断层.
位于中國西南的小江(Xiaojiang)斷裂帶作為康定(Kangding)斷裂帶的南段,在青藏塊體嚮SE方嚮擠齣的過程中起著重要的作用.根據斷錯地貌以及這些斷錯地貌14C年代或熱釋光年代,推算瞭小江斷裂帶第四紀晚期的左鏇走滑速率.小江斷裂帶可以分為3段,其中段由平行的兩條斷層組成.西支斷層和東支斷層的左鏇走滑速率分彆為7.0~9.0mm/yr和6.0~7.5mm/yr.簡單相加,就可以推算齣小江(Xiaojiang)斷裂帶總的左鏇走滑速率為13.0~16.5mm/yr,與康定斷裂帶北段的鮮水河(Xianshuihe)斷層的走滑速率大緻相噹,約等于康定(Kangding)斷裂帶中段的安寧河(Anninghe)斷層及則木河(Zemuhe)斷層的兩倍.這箇結果可能暗示瞭在康定斷裂帶中段,可能存在著其他斷層以解消另外一半的滑動速率.最有可能的斷層是位于康定斷裂帶中段以東幾十公裏的普雄河-佈拖(Puxionghe-Butuo)斷層.
위우중국서남적소강(Xiaojiang)단렬대작위강정(Kangding)단렬대적남단,재청장괴체향SE방향제출적과정중기착중요적작용.근거단착지모이급저사단착지모14C년대혹열석광년대,추산료소강단렬대제사기만기적좌선주활속솔.소강단렬대가이분위3단,기중단유평행적량조단층조성.서지단층화동지단층적좌선주활속솔분별위7.0~9.0mm/yr화6.0~7.5mm/yr.간단상가,취가이추산출소강(Xiaojiang)단렬대총적좌선주활속솔위13.0~16.5mm/yr,여강정단렬대북단적선수하(Xianshuihe)단층적주활속솔대치상당,약등우강정(Kangding)단렬대중단적안저하(Anninghe)단층급칙목하(Zemuhe)단층적량배.저개결과가능암시료재강정단렬대중단,가능존재착기타단층이해소령외일반적활동속솔.최유가능적단층시위우강정단렬대중단이동궤십공리적보웅하-포타(Puxionghe-Butuo)단층.
The Xiaojiang fault is the southern portion of the Kangding fault zone, which is a noticeable active fault in southwest China and plays an important role in the left-lateral extrusion of the Tibetan Plateau. We determined average slip rates of the Xiaojiang fault, on the basis of offset landforms that were precisely mapped and dated by radiocarbon or thermoluminescence methods. The Xiaojiang fault consists of two subparallel fault strands in its middle segment; the average left-lateral slip rates on the west and east strands were determined to be 7.0~9.0mm/yr and 6.0~7.5mm/yr, respectively. Thus, the total slip rate on the Xiaojiang fault amounts to 13.0~16.5mm/yr. This value is approximately equal to that on the Xianshuihe fault, the northern part of the Kangding fault zone, and about twice as high as that on the Anninghe and Zemuhe faults, the middle part of the Kangding fault zone. Our results suggest that there must be other active faults that accommodate the missing slip in the middle of the Kangding fault zone; the most probable candidate may be the Puxionghe-Butou fault zone located several ten kilometers to the east of the middle segment.0041, China[=4) Seismological Bureau of Yunnan Province, Kunming 65