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Information Journal Paper

Title

DEPTH TO BEDROCK DETERMINATION USING GRAVIMETRIC METHOD IN THE SOUTH PART OF ZAGROS REGION

Pages

  61-69

Abstract

 Gravimetry is an effective and almost inexpensive approach to assess the DEPTH TO BEDROCK in sedimentary basins. In this research a gravity data sets located in south part of Zagros has been applied. The sedimentary deposits covered the top of a syncline which is located between two anticlines. An iterative gravity inversion method (Jachens and Moring, 1990) has been applied to determine the depth of sedimentary deposits in the region. In order to test the accuracy and practicability of this method both 2dimensional and 3dimensional synthesizeddata has been applied. For determining the surface density and density-based zoning of the region aNettelton Analysis has been used. Geological andgeomorphological evidences almost confirm the determined depth results.

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    APA: Copy

    MOTESHAREI, A., & ZOMORODIAN, H.. (2008). DEPTH TO BEDROCK DETERMINATION USING GRAVIMETRIC METHOD IN THE SOUTH PART OF ZAGROS REGION. IRANIAN JOURNAL OF GEOPHYSICS, 1(1), 61-69. SID. https://sid.ir/paper/133805/en

    Vancouver: Copy

    MOTESHAREI A., ZOMORODIAN H.. DEPTH TO BEDROCK DETERMINATION USING GRAVIMETRIC METHOD IN THE SOUTH PART OF ZAGROS REGION. IRANIAN JOURNAL OF GEOPHYSICS[Internet]. 2008;1(1):61-69. Available from: https://sid.ir/paper/133805/en

    IEEE: Copy

    A. MOTESHAREI, and H. ZOMORODIAN, “DEPTH TO BEDROCK DETERMINATION USING GRAVIMETRIC METHOD IN THE SOUTH PART OF ZAGROS REGION,” IRANIAN JOURNAL OF GEOPHYSICS, vol. 1, no. 1, pp. 61–69, 2008, [Online]. Available: https://sid.ir/paper/133805/en

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