Architecture of tectonic and crustal structure of the middle marmara sub-basin and its surroundings using gravity data

被引:0
|
作者
Abdurrahman Yasir Parlak
Ali Elmas
机构
[1] Karadeniz Technical University,Department of Geophysical Engineering
来源
Carbonates and Evaporites | 2023年 / 38卷
关键词
Total horizontal derivative; Marmara sea basin; Discontinuities; Normalized full gradient; Isostatic Moho;
D O I
暂无
中图分类号
学科分类号
摘要
To study the tectonic and crustal structure of the Middle Marmara Sub-basin and its surroundings, gravity data obtained from the Earth Gravitational Model (EGM08) were analyzed using Radially Averaged Amplitude Spectrum, Total Horizontal Derivative (THD), Parker-Oldenburg (PO) inversion, Normalized Full Gradient (NFG) and Isostatic Analysis techniques. While positive gravity anomalies are observed on the Çınarcık and West Marmara sub-basins on the Marmara Sea Basin, the reason for the negative gravity anomalies observed on the Middle Marmara Sub-basin is one of the objectives of this study. Moreover, the earthquake epicenters are concentrated in the central part of the Main Marmara Fault (MMF) on the Middle Marmara Sub-basin, while sparse in the eastern part of the MMF in the eastern part of the sub-basin. To investigate the causes of these, first of all, the average depth values of the in-sediments, basement, Conrad and Moho discontinuities of the study area were calculated using the radially averaged amplitude spectrum of the Bouguer gravity data. The THD technique was used to display the discontinuity limits at different levels. As a result of the THD calculations, the continuity of the MMF in Middle Marmara Sub-basin could not be observed as a strait fault. It has been interpreted that this fault consists of a series of small faults in this area. Also, the basement topography of the study area was calculated with the inverse solution, hence basement depth varies between 2.8 and 7.4 km. The differences between the Gravimetric Moho and the Isostatic Moho were calculated, and areas with high and low seismic activity were mapped. With this study, it has been concluded that the equilibrium state of the crust has not yet formed around the Middle Marmara Sub-basin and its surroundings. Moreover, the negative gravity anomalies are caused by the collapse of the crust around this sub-basin.Please confirm if the author names are presented accurately and in the correct sequence. Author 1 Given name: [Abdurrahman Yasir] Last name [Parlak]. Also, kindly confirm the details in the metadata are correct.I confirm the author names are presented accurately and in the correct sequence. Author 1 Given name: [Abdurrahman Yasir] Last name [Parlak]. Also, I confirm the details in the metadata are correct.
引用
收藏
相关论文
共 50 条
  • [21] Crustal structure and deformation under the Longmenshan and its surroundings revealed by receiver function data
    Sun, Ya
    Liu, Jianxin
    Zhou, Keping
    Chen, Bo
    Guo, Rongwen
    PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 2015, 244 : 11 - 22
  • [22] Crustal Structure beneath Yinggehai Basin and Adjacent Hainan Island, and Its Tectonic Implications
    吴世敏
    丘学林
    周蒂
    曾刚平
    夏戡原
    叶三余
    Journal of Earth Science, 2009, (01) : 13 - 26
  • [24] Crustal Structure beneath Yinggehai Basin and Adjacent Hainan Island, and Its Tectonic Implications
    Wu Shimin
    Qiu Xuelin
    Zhou Di
    Zeng Gangping
    Xia Kanyuan
    Ye Sanyu
    JOURNAL OF EARTH SCIENCE, 2009, 20 (01) : 13 - 26
  • [25] Simulating hydrological processes in a sub-basin of the Mekong using GBHM and RS data
    Wang, Wei
    Lu, Hui
    Yang, Dawen
    Gao, Bin
    Jiao, Yang
    Pang, Zhiguo
    REMOTE SENSING AND GIS FOR HYDROLOGY AND WATER RESOURCES, 2015, 368 : 221 - 226
  • [26] The subsurface structure of the Chalco sub-basin (Mexico City) inferred from geophysical data
    Campos-Enríquez, J. O.
    Delgado-Rodríguez, O.
    Chávez-Segura, R.
    Gómez-Contreras, P.
    Flores-Márquez, E. L.
    Birch, F.S.
    Geophysics, 1997, 62 (01): : 23 - 35
  • [27] Crustal architecture of the Wilkes Subglacial Basin in East Antarctica, as revealed from airborne gravity data
    Jordan, T. A.
    Ferraccioli, F.
    Armadillo, E.
    Bozzo, E.
    TECTONOPHYSICS, 2013, 585 : 196 - 206
  • [28] The subsurface structure of the Chalco sub-basin (Mexico City) inferred from geophysical data
    CamposEnriquez, JO
    DelgadoRodriguez, O
    ChavezSegura, R
    GomezContreras, P
    FloresMarquez, EL
    Birch, FS
    GEOPHYSICS, 1997, 62 (01) : 23 - 35
  • [29] Gravity–magnetic appraisal at the interface of Cuddapah Basin and Nellore Schist Belt (NSB) for shallow crustal architecture and tectonic settings
    Shuva Shankha Ganguli
    Sanjit Kumar Pal
    J V Rama Rao
    B Sunder Raj
    Journal of Earth System Science, 2020, 129
  • [30] S-wave velocity structure and tectonic implications of the northwestern sub-basin and Macclesfield of the South China Sea
    Xiaodong Wei
    Aiguo Ruan
    Jiabiao Li
    Xiongwei Niu
    Zhenli Wu
    Weiwei Ding
    Marine Geophysical Research, 2017, 38 : 125 - 136