高原地震
高原地震
고원지진
EARTHQUAKE RESEARCH IN PLATEAU
2012年
4期
25-30,43
,共7页
汶川地震%活动断裂%灾害%地表破裂
汶川地震%活動斷裂%災害%地錶破裂
문천지진%활동단렬%재해%지표파렬
Wenchuan earthquake%Active fault%Disaster%Surface rupture
发生在龙门山断裂带上的汶川Ms8.0级地震引起的地表破裂主要分布在北川-映秀断裂带和江油-灌县断裂带上,尤其是沿前者发育了长达240km的地表破裂带,造成了重大的人员与财产损失。灾害发生的原因是多方面的:地震的震级大;震中所处地区构造发育,地质环境极为脆弱;人口较为密集,城镇的场地普遍狭窄,空间有限等。但是,断层的作用是决定性的,且在不同地段表现出了明显的差异性,导致了不同类型的地震灾害。对于断层的避让与设防问题考虑不足,放大了本次地震的灾害效应。
髮生在龍門山斷裂帶上的汶川Ms8.0級地震引起的地錶破裂主要分佈在北川-映秀斷裂帶和江油-灌縣斷裂帶上,尤其是沿前者髮育瞭長達240km的地錶破裂帶,造成瞭重大的人員與財產損失。災害髮生的原因是多方麵的:地震的震級大;震中所處地區構造髮育,地質環境極為脆弱;人口較為密集,城鎮的場地普遍狹窄,空間有限等。但是,斷層的作用是決定性的,且在不同地段錶現齣瞭明顯的差異性,導緻瞭不同類型的地震災害。對于斷層的避讓與設防問題攷慮不足,放大瞭本次地震的災害效應。
발생재룡문산단렬대상적문천Ms8.0급지진인기적지표파렬주요분포재북천-영수단렬대화강유-관현단렬대상,우기시연전자발육료장체240km적지표파렬대,조성료중대적인원여재산손실。재해발생적원인시다방면적:지진적진급대;진중소처지구구조발육,지질배경겁위취약;인구교위밀집,성진적장지보편협착,공간유한등。단시,단층적작용시결정성적,차재불동지단표현출료명현적차이성,도치료불동류형적지진재해。대우단층적피양여설방문제고필불족,방대료본차지진적재해효응。
The Ms8.0 Wenchuan earthquake that occurred on the Longmenshan area had produced two surface rupture faults: Beiehuan-Yingxiu fault and Jiangyou-Guanxian fault. Especially along the first fault, the earth- quake produced a 240 kin-long rupture zone, causing huge casualties and property losses. There were many rea- sons for this disaster : the earthquake magnitude was very high, reaching Ms8.0 ; the epicenter region was in tec- tonic development, so its geological environment was very fragile; the town had a relatively dense population but a generally narrow venue and limited space. However, the role of faults was decisive, which in different loca- tions showed significant differences, leading to the emergence of different types of earthquake damages. Lack of consideration for fault avoidance and fortification amplified the disastrous effects of the earthquake.