Imagıng the Crustal Structure of the Southern Marmara Region (Turkey) Using Aeromagnetic and Gravitational Data

Muhammet Ali Aygün; Ahmet Sinan Demirel

Makale detayları

Imagıng the Crustal Structure of the Southern Marmara Region (Turkey) Using Aeromagnetic and Gravitational Data

Yazarlar:

Muhammet Ali Aygün | Ahmet Sinan Demirel

Yayıncı:

Istanbul University

Ana Başlıklar:

Geological Sciences and Engineering (Other)

Dergi:

International Journal of Environment and Geoinformatics Vol.11 Issue 4, pp.101-108

Belge Tipi:

Makale

Yayın Tarihi:

12/2024

Belge Dili:

İngilizce

Document ID (Org No.):

2001328487

pISSN:

2148-9173

Anahtar kelimeler:

Özet:

 In this study, discontinuities and major tectonic boundaries are interpreted in and around the South Marmara Region through the analysis of airborne Bouguer gravity and magnetic anomalies. Radial average power spectrum RAPS and band-pass filtering techniques are employed for the separation of long and short wavelengths. The application of RASP to the entire study area has yielded the detection of four depth segments, which have been employed in conjunction with tilt derivatives for the estimation of structural depth. Furthermore, the radial average depths of these depth segments are 30.5 km, 11.6 km, 3.2 km and 0.32 km. This study aims to gain insight into the crustal characteristics of the South Marmara region through the utilisation of geophysical data, with a particular focus on the YDABCAG-198Y231G grid data obtained through the digitisation of analogue data from the Aegean region. The relative merits and limitations of general and developed models will be discussed.

 In this study, discontinuities and major tectonic boundaries are interpreted in and around the South Marmara Region through the analysis of airborne Bouguer gravity and magnetic anomalies. Radial average power spectrum RAPS and band-pass filtering techniques are employed for the separation of long and short wavelengths. The application of RASP to the entire study area has yielded the detection of four depth segments, which have been employed in conjunction with tilt derivatives for the estimation of structural depth. Furthermore, the radial average depths of these depth segments are 30.5 km, 11.6 km, 3.2 km and 0.32 km. This study aims to gain insight into the crustal characteristics of the South Marmara region through the utilisation of geophysical data, with a particular focus on the YDABCAG-198Y231G grid data obtained through the digitisation of analogue data from the Aegean region. The relative merits and limitations of general and developed models will be discussed.

 In this study, discontinuities and major tectonic boundaries are interpreted in and around the South Marmara Region through the analysis of airborne Bouguer gravity and magnetic anomalies. Radial average power spectrum RAPS and band-pass filtering techniques are employed for the separation of long and short wavelengths. The application of RASP to the entire study area has yielded the detection of four depth segments, which have been employed in conjunction with tilt derivatives for the estimation of structural depth. Furthermore, the radial average depths of these depth segments are 30.5 km, 11.6 km, 3.2 km and 0.32 km. This study aims to gain insight into the crustal characteristics of the South Marmara region through the utilisation of geophysical data, with a particular focus on the YDABCAG-198Y231G grid data obtained through the digitisation of analogue data from the Aegean region. The relative merits and limitations of general and developed models will be discussed.

 In this study, discontinuities and major tectonic boundaries are interpreted in and around the South Marmara Region through the analysis of airborne Bouguer gravity and magnetic anomalies. Radial average power spectrum RAPS and band-pass filtering techniques are employed for the separation of long and short wavelengths. The application of RASP to the entire study area has yielded the detection of four depth segments, which have been employed in conjunction with tilt derivatives for the estimation of structural depth. Furthermore, the radial average depths of these depth segments are 30.5 km, 11.6 km, 3.2 km and 0.32 km. This study aims to gain insight into the crustal characteristics of the South Marmara region through the utilisation of geophysical data, with a particular focus on the YDABCAG-198Y231G grid data obtained through the digitisation of analogue data from the Aegean region. The relative merits and limitations of general and developed models will be discussed.

Makale detayları

Imagıng the Crustal Structure of the Southern Marmara Region (Turkey) Using Aeromagnetic and Gravitational Data

Yazarlar:

Muhammet Ali Aygün | Ahmet Sinan Demirel

Yayıncı:

Istanbul University

Ana Başlıklar:

Geological Sciences and Engineering (Other)

Dergi:

International Journal of Environment and Geoinformatics Vol.11 Issue 4, pp.101-108

Belge Tipi:

Makale

Yayın Tarihi:

12/2024

Belge Dili:

İngilizce

Document ID (Org No.):

2001328487

pISSN:

2148-9173

airbourne gravity

airbourne magnetic

tilt depth

radially averaged sliced depth

Sayı

Makale detayları

Imagıng the Crustal Structure of the Southern Marmara Region (Turkey) Using Aeromagnetic and Gravitational Data

Yazarlar: Muhammet Ali Aygün | Ahmet Sinan Demirel

Yayıncı: Istanbul University

Ana Başlıklar: Geological Sciences and Engineering (Other)

Dergi: International Journal of Environment and Geoinformatics Vol.11 Issue 4, pp.101-108

Belge Tipi: Makale

Yayın Tarihi: 12/2024

Belge Dili: İngilizce

Document ID (Org No.): 2001328487

pISSN: 2148-9173

airbourne gravity

airbourne magnetic

tilt depth

radially averaged sliced depth

Sayı

Yazarlar:

Muhammet Ali Aygün | Ahmet Sinan Demirel

Yayıncı:

Istanbul University

Ana Başlıklar:

Geological Sciences and Engineering (Other)

Dergi:

International Journal of Environment and Geoinformatics Vol.11 Issue 4, pp.101-108

Belge Tipi:

Makale

Yayın Tarihi:

12/2024

Belge Dili:

İngilizce

Document ID (Org No.):

2001328487

pISSN:

2148-9173