J4 ›› 2010, Vol. 40 ›› Issue (5): 1170-1176.

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Study on Geology and Geophysics on Structural Units of Hulin Basin in Heilongjiang Province

ZHANG Feng-xu1, ZHANG Xing-zhou2, ZHANG Feng-qin3, SUN Jia-peng2, QIU Dian-ming4, XUE Jin5   

  1. 1.College of GeoExploration Science and Technology, Jilin University, Changchun 130026, China;
    2.College of Earth Sciences,Jilin University, Changchun 130061, China;
    3.College of Physics, Jilin University, Changchun 130023, China;
    4.Editorial Department of Journal| Jilin University, Changchun 130026, China;
    5.Engineering Geophysical Exploration Institute of Jiangsu Province, Nanjing 210008, China
  • Received:2009-11-05 Online:2010-09-26 Published:2010-09-26

Abstract:

Based on the cosine transform method, and using the method of upward continuation and computed base depth of the basin using the inverse technique of even (density) and single interface, the authors had processed the Hulin basin Bouguer gravity anomalies and inversed the base depth. At the same time, by analyzing integrated interpretation results of gravity and magnetotelluric sounding profile in Hulin basin and neighbouring geologic information in Russia, We studied differences of underlying structure between south and north of the basin reflected by geology and geophysics, and redistricted its structural units. It is shown that the south fracture of Dunmi fault, which was composed of two faults, is vertical and strike-slip fault, it controls strike-slip movement of its bilateral fault block and the formation and evolution of the basin. If let Dunmi south fault as dividing line, the Hulin basin can be divided into two basins, i.e. south basin and north basin, and their geology and geophysics properties are totally different. The north basin is part of large Sanjiang basin, whereas the south basin is an independent basin system.

Key words: Hulin basin, gravity anomaly, structure unit, Dunmi south fault, strike-slip fault, geology, geophysics

CLC Number: 

  • P631.1
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