城市地质
城市地質
성시지질
URBAN GEOLOGY
2015年
2期
83-86
,共4页
刘博%陈天红%冯欣%续远超%任柄璋%陈广宇%宋丙剑
劉博%陳天紅%馮訢%續遠超%任柄璋%陳廣宇%宋丙劍
류박%진천홍%풍흔%속원초%임병장%진엄우%송병검
阿巴嘎旗%白音图噶%航磁%断裂构造
阿巴嘎旂%白音圖噶%航磁%斷裂構造
아파알기%백음도갈%항자%단렬구조
Abga Banner%Baiyintuga area%Aeromagnetic%Faulted structures
内蒙古阿巴嘎旗白音图嘎地区为浅覆盖区,地表构造形迹难以识别。笔者以最新的高精度航磁资料为依据,论述了区内深大断裂的磁场特征,并对航磁在断裂构造解疑中的应用进行了探讨。根据区内构造磁异常特征,在航磁△T化极垂向一次导数基础上,全区共解译断裂构造15条。构造方向主要为北东、北西方向,其中F1、F2、F3、F4、F7、F8、F9位于白音图嘎幅,岩性主要为宝力高庙组,为基岩出露区,脉岩比较发育,为花岗斑岩脉、正长斑岩脉,地表出露岩脉主要呈北西向,与航磁解译构造较为吻合,经向上延拓后构造不明显,显示底部为同一岩性基底;F5、F14、F15经向上延拓构造变得更加清晰,推断该构造由深部大的构造引起。
內矇古阿巴嘎旂白音圖嘎地區為淺覆蓋區,地錶構造形跡難以識彆。筆者以最新的高精度航磁資料為依據,論述瞭區內深大斷裂的磁場特徵,併對航磁在斷裂構造解疑中的應用進行瞭探討。根據區內構造磁異常特徵,在航磁△T化極垂嚮一次導數基礎上,全區共解譯斷裂構造15條。構造方嚮主要為北東、北西方嚮,其中F1、F2、F3、F4、F7、F8、F9位于白音圖嘎幅,巖性主要為寶力高廟組,為基巖齣露區,脈巖比較髮育,為花崗斑巖脈、正長斑巖脈,地錶齣露巖脈主要呈北西嚮,與航磁解譯構造較為吻閤,經嚮上延拓後構造不明顯,顯示底部為同一巖性基底;F5、F14、F15經嚮上延拓構造變得更加清晰,推斷該構造由深部大的構造引起。
내몽고아파알기백음도알지구위천복개구,지표구조형적난이식별。필자이최신적고정도항자자료위의거,논술료구내심대단렬적자장특정,병대항자재단렬구조해의중적응용진행료탐토。근거구내구조자이상특정,재항자△T화겁수향일차도수기출상,전구공해역단렬구조15조。구조방향주요위북동、북서방향,기중F1、F2、F3、F4、F7、F8、F9위우백음도알폭,암성주요위보력고묘조,위기암출로구,맥암비교발육,위화강반암맥、정장반암맥,지표출로암맥주요정북서향,여항자해역구조교위문합,경향상연탁후구조불명현,현시저부위동일암성기저;F5、F14、F15경향상연탁구조변득경가청석,추단해구조유심부대적구조인기。
Baiyintuga area, the Abga Banner, Inner Mongolia is a shallow covering area of geological structures, where the surface structural features are indiscernible. This paper provides a detailed description of the magnetic field characteristics of deep faults in this area and discussion on the application of the aeromagnetic in faulted structure interpretation based on the latest high-precision aeromagnetic data. According to the structure characteristics of magnetic anomaly mentioned above, 15 faulted structures are distinguished in this area based on first derivative of aeromagnetic ΔT vertical directions. The main structures extend as north-east and north-west directions. As for the faults such as F1、F2、F3、F4、F7、F8、F9, located in Baiyintuga area, the lithology in the faulted area mainly belongs to Baoligaomiao Fm. They are rock outcropped areas with well-developed vein rock, among which are principally granite porphyry veins and syenite porphyry veins. The surface exposed dikes are mainly in the north-west direction, which are similar to the aeromagnetic interpretation structure. While the structures are upward extending, they become indistinct, which indicates they have the same base-rock at the bottom. But as for the faults of F5、F14、F15 have much clearer upward continuation, so these faults may be caused by the large fracture in the deep.