normal fault zone 中文意思是什麼
normal fault zone
解釋
正斷層帶-
The fault zone passes through the offshore between the changdong islands and the dazhudao island, and consists of a group of nw trending faults, which are dominated by normal and reverse slips with strike - slip component
該斷裂帶由一系列北西走向的次級斷層組成,主體在長島至大竹島之間的海域,多數斷層以正斷兼有走滑運動為主,部分斷層具有逆沖運動性質。 -
Typical examples include the xidatan palaeo - seismic fracture zone, seismic fracture zone of the kunlun ms 8. 1 earthquake occurred in november 14, 2001, the south hohxil palaeo - seismic fracture zone, seismic fracture zone of the bengcuo ms 8. 0 earthquake occurred in 1951 and seismic fracture zones along normal fault in east of the nyainqentanglha mts. caused by jiuzila ms 7. 5 earthquake occurred in 1952 and yangbajain ms 8. 0 earthquake occurred in 1411
典型地震破裂包括西大灘古地震破裂、昆侖山南緣地震破裂、可可西里古地震破裂、崩錯地震破裂、谷露盆西地震破裂、羊八井當雄盆西地震破裂;地震破裂規模大,產狀穩定,與地震鼓包、地震陡坎、地震凹陷有序組合,是地表構造變形的重要形式,屬內動力成因地裂縫。 -
Several normal faults within the hainan fault zone constitute a fault - step zone and form a narrow and steep zone, which controlled the development and distribution of depositional systems in this area
研究認為,海南斷裂帶的幾個北掉斷層構成斷階帶,形成湖盆邊緣陡且窄的地貌特點,控制了該區沉積體系的展布規律。 -
The extensional activities of hefei basin occurred in the period between late cretaceous and paleogene. as a result, the extensional normal faults were took place along the pre - existing nearly ew faults and the tan - lu fault zone. the deposition of half - graben was formed
合肥盆地的伸展活動發生於晚白堊世至早第三紀,伸展活動是疊加在前兩期走滑構造之上,形成了以半地塹式楔形為主的沉積。
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