CAJ | 학술논문

青藏高原东北缘构造变形的研究是认识高原隆起过程、机制和印度-欧亚板块碰撞远程效应的重要途径.柴达木盆地是印度-欧亚板块碰撞后南北向挤压应力为动力背景的高原东北部内陆盆地,沉积物主要来自于周边山地,完整的保存了新生代以来高原隆升的详细记录.通过柴达木盆地东北部瑙格剖面精细古地磁及构造旋转研究发现,20.1～15.1Ma以及15.1～8.2Ma柴达木盆地分别发生了9.7°±7.4°和6.4°±4.4°的顺时针旋转,约8.2Ma后,柴达木盆地东北部瑙格地区发生了16°±7.5°的逆时针快速旋转.通过分析认为,前两次的顺时针构造旋转事件可能与阿尔金断裂的左旋走滑有关.而约8.2Ma以来的逆时针旋转事件属于柴达木盆地东北部瑙格地区的局部旋转,可能与温泉断裂的右旋走滑有关,说明青藏高原东北部在昆仑山、阿尔金山和祁连山三条巨型断裂系左旋相对运动的宏观控制下形成的NNW向温泉右旋走滑断裂开始走滑的年代为约8Ma.
청장고원동북연구조변형적연구시인식고원륭기과정、궤제화인도-구아판괴팽당원정효응적중요도경.시체목분지시인도-구아판괴팽당후남북향제압응력위동력배경적고원동북부내륙분지,침적물주요래자우주변산지,완정적보존료신생대이래고원륭승적상세기록.통과시체목분지동북부노격부면정세고지자급구조선전연구발현,20.1～15.1Ma이급15.1～8.2Ma시체목분지분별발생료9.7°±7.4°화6.4°±4.4°적순시침선전,약8.2Ma후,시체목분지동북부노격지구발생료16°±7.5°적역시침쾌속선전.통과분석인위,전량차적순시침구조선전사건가능여아이금단렬적좌선주활유관.이약8.2Ma이래적역시침선전사건속우시체목분지동북부노격지구적국부선전,가능여온천단렬적우선주활유관,설명청장고원동북부재곤륜산、아이금산화기련산삼조거형단렬계좌선상대운동적굉관공제하형성적NNW향온천우선주활단렬개시주활적년대위약8Ma.
Tectonic deformation research of the NE Tibetan Plateau is a good approach in understanding the Tibetan Plateau's uplift,mechanism, Indian-Eurasian collision influence. The Qaidam basin is the closed inland basin in the NE Tibetan Plateau. It is surrounded by the Kunlun fault belt(the southern boundary), the Altyn fault belt(the western boundary), the Qilian fault belt(the northern boundary), the Wenquan fault belt(the eastern boundary) and contains possibly thickest(about 12 km)continuous sequence of Cenozoic sedimentary rocks.The sequence contains considerable information on the history of Tibetan uplift.Here we report a high-resolution paleomagnetic and tectonic rotation study of the well exposed 3237m Naoge section in the northeastern Qaidam Basin,where we found a 9.7°±7.4 °clockwise tectonic rotation from 20.1Ma to 15.1Ma, a 6.4°±4.4 °clockwise tectonic rotation from 15.1Ma to 8.2Ma, a 16°±7.5 °counterclockwise tectonic rotation after 8.2Ma. Two times of the clockwise tectonic rotation because of the Altyn Tagh sinistral shear strain propagated to Qaidam Basin,they are representative of the Qaidam block's rotation. A counterclockwise tectonic rotation because of the right-lateral strike-slip displacement of the Wenquan fault,it representative of the Naoge area's rotation,and it showed that the beginning time of the NNW strike right-lateral Wenquan fault which is controled by the left-lateral strike-slip East-Kunlun fault ,the left-lateral strike-slip Altyn Tagh fault and the left-lateral strike-slip Qilian fault was about at 8 Ma.