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
  • [41] Gravity anomalies and deep crustal structure of the Ordos basin-middle Qinling orogen-eastern Sichuan basin
    Wang Qian-Shen
    Teng Ji-Wen
    Zhang Yong-Qian
    Pi Jiao-Long
    CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, 2015, 58 (02): : 532 - 541
  • [42] Crustal structure of the northwestern sub-basin, South China Sea: Results from a wide-angle seismic experiment
    ZhenLi Wu
    JiaBiao Li
    AiGuo Ruan
    Hai Lou
    WeiWei Ding
    XiongWei Niu
    XiBing Li
    Science China Earth Sciences, 2012, 55 : 159 - 172
  • [43] Tectonic subsidence modelling of the Polish Basin in the light of new data on crustal structure and magnitude of inversion
    Stephenson, RA
    Narkiewicz, M
    Dadlez, R
    van Wees, JD
    Andriessen, P
    SEDIMENTARY GEOLOGY, 2003, 156 (1-4) : 59 - 70
  • [44] DETERMINATION OF FLOOD RISK IN SAKARYA SUB-BASIN USING REMOTELY SENSED DATA AND GIS
    Ozcan, Orkan
    Musaoglu, Nebiye
    Seker, Dursun Zafer
    Tanik, Aysegul
    FRESENIUS ENVIRONMENTAL BULLETIN, 2008, 17 (11B): : 1964 - 1970
  • [45] Low grade metamorphism in the Lalsot-Bayana sub-basin of the North Delhi Fold Belt and its tectonic implication
    Muntazir Mehdi
    Santosh Kumar
    Naresh C. Pant
    Journal of the Geological Society of India, 2015, 85 : 397 - 410
  • [46] Gravity-magnetic appraisal at the interface of Cuddapah Basin and Nellore Schist Belt (NSB) for shallow crustal architecture and tectonic settings
    Ganguli, Shuva Shankha
    Pal, Sanjit Kumar
    Rao, J. V. Rama
    Raj, B. Sunder
    JOURNAL OF EARTH SYSTEM SCIENCE, 2020, 129 (01)
  • [47] Low Grade Metamorphism in the Lalsot-Bayana Sub-basin of the North Delhi Fold Belt and its Tectonic Implication
    Mehdi, Muntazir
    Kumar, Santosh
    Pant, Naresh C.
    JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA, 2015, 85 (04) : 397 - 410
  • [48] Cenozoic tectonic evolution of the eastern Liaodong Bay sub-basin, Bohai Bay basin, eastern China-Constraints from seismic data
    Luo, Jingshuang
    Sun, Yonghe
    Wang, Yougong
    Xie, Zhaohan
    Meng, Lingdong
    MARINE AND PETROLEUM GEOLOGY, 2021, 134
  • [49] Crustal Electrical Structure of the Zhaheba Complex Imaged by Magnetotelluric Data and Its Tectonic Implications
    Zhang, Pingchuan
    Yu, Changqing
    Zeng, Xiangzhi
    APPLIED SCIENCES-BASEL, 2021, 11 (21):
  • [50] Exploring climate variability and its impact on drought occurrence: Evidence from Godavari Middle sub-basin, India
    Masroor, Md
    Rehman, Sufia
    Avtar, Ram
    Sahana, Mehebub
    Ahmed, Raihan
    Sajjad, Haroon
    WEATHER AND CLIMATE EXTREMES, 2020, 30