摘要
文章以新疆塔里木盆地西缘高精度航磁测量的成果资料作为基础数据,对塔里木盆地西缘区域磁场特征与大地构造单元的关系进行了研究。依据航磁资料,划出3条深断裂(即磁场区分界线),分析了深断裂在航磁、地质资料上反映的特征,其中F_1断裂和F_2断裂与地质上划定的断裂基本吻合,F_3断裂部分吻合,对其空间位置提出了新的认识。将研究区划分为4个特征各异的磁场区,并进一步划分了二级磁场区,从磁场特征、地层分布、大地构造位置、基底性质、区域场成因等方面进行了阐述。
Based on high-precision aeromagnetic data in the western margin of Tarim Basin,this paper studies the intrinsic relationship between the characteristics of regional magnetic field and the division of geotectonic units.According to aeromagnetic data,three deep faults(demarcation lines of regional magnetic fields)are delineated.The characteristics of the faults reflected in aeromagnetic and geological data are analyzed.Fault F_1 and F_2 are basically identical with the geologically delineated faults.F_3 is partly identical and a new understanding of its spatial location is put forward.This area is divided into four magnetic field regions with different characteristics and sub-magnetic fields are divided and the magnetic field characteristics,strata distribution,geotectonic location,basement properties and regional field genesis are discussed.
引文
[1]向鼎璞.新疆大地构造轮廓[J].地质论评,1959(2):49-59.
[2]胡冰,王景斌,高振家,等.新疆大地构造的几个问题[J].地质学报,1964,44(2):156-170.
[3]陈哲夫,梁云海.新疆多旋回构造与板块运动[J].新疆地质,1991,9(2):95-107.
[4]张良臣,刘德权,等.中国新疆优势金属矿产成矿规律[M].北京:地质出版社,2006.
[5]董连慧,屈迅,朱志新,等.新疆大地构造演化与成矿[J].新疆地质,2010,28(4):351-357.
[6]卢书炜,杜凤军,任建德,等.库尔干幅1/250000区域地质调查报告[R].郑州:河南省地质调查院,2005.
[7]卢书炜,方怀宾,杜凤军,等.中华人民共和国区域地质调查报告(1∶250000艾提开尔丁萨依幅、英吉沙县幅)[M].武汉:中国地质大学出版社有限责任公司,2013.
[8]高锐,肖序常,高弘,等.西昆仑-塔里木-天山岩石圈深地震探测综述[J].地质通报,2002,21(1):11-18.