Abstract
The rock samples of different ages were collected at the Armutlu Peninsula and were subjected to the geochemical analysis. The magnetic susceptibility measurements were performed either in situ in the study area using MS-2 sensor and in the laboratory. The magnetic susceptibility map and the magnetic susceptibility-depth profiles of the investigation area were figured out
References
- AKARTUNA M., 1968. Armutlu Yarımadasının Jeolojisi : İÜFF Monografi, 20, 120 s.
- ANDREW P. ROBERTS., 2006. High-resolution magnetic analysis of sediment cores: Strengths, limitations and strategies for maximizing the value of long-core magnetic data Physics of The Earth and Planetary Interiors, 156,162-178.
- AYDIN A., GELİŞLİ K., 1996. Magnetic studies in Saruhan-Bayburt skarn zone (in Turkish).Saruhan-Bayburt Skarn Zonunda Manyetik Çalışmalar, Jeofizik, 10,40-49.
- DEARİNG J.A., HAY K.L., BABAN S.M.J., HUDDLESTON A.S., WELLİNGTON E.M.H.,
- LOVELAND P.J., 1996. Magnetic susceptibility of soil: An Evaluation of Conflicting Theories using a national data set, Geophys J Int;127:728-734.
- LECOANET H., LÉVESQUE F., SEGUNA S., 1999. Magnetic susceptibility in environmental applications: comparison of field probes. Phys. Earth Planet. Inter. 115, 191 – 204.
- MULLINS C.E., TITE M.S., 1973. Magnetic viscosity, quadrature susceptibility and frequency dependence of susceptibility in single–domain assemblages of magnetite and maghaemite. J. Geophys. Res. 78, 804-809.
- STEFANIE A. BRACHFELD., 2006. High-field magnetic susceptibility (χHF) as a proxy of biogenic sedimentation along the Antarctic Peninsula, Physics of The Earth and Planetary Interiors , 156, 274-282.
Abstract
Armutlu Yarımadası’nda yer alan çeşitli yaşlara ait kaya örnekleri toplanarak laboratuarda jeokimyasal analizlere tabii tutulmuştur. Manyetik duyarlık ölçümleri hem yerinde hem de laboratuarda gerçeklenmiş, bölgenin manyetik duyarlık haritası ve manyetik duyarlık-derinlik değişim profilleri çıkartılmıştır. Bu amaçla bölgenin değişik yörelerinden yönlü el numuneleri alınmış ve ölçümleri yapılmıştır. Ölçüm için MS- 2 ölçüm cihazı kullanılmıştır
References
- AKARTUNA M., 1968. Armutlu Yarımadasının Jeolojisi : İÜFF Monografi, 20, 120 s.
- ANDREW P. ROBERTS., 2006. High-resolution magnetic analysis of sediment cores: Strengths, limitations and strategies for maximizing the value of long-core magnetic data Physics of The Earth and Planetary Interiors, 156,162-178.
- AYDIN A., GELİŞLİ K., 1996. Magnetic studies in Saruhan-Bayburt skarn zone (in Turkish).Saruhan-Bayburt Skarn Zonunda Manyetik Çalışmalar, Jeofizik, 10,40-49.
- DEARİNG J.A., HAY K.L., BABAN S.M.J., HUDDLESTON A.S., WELLİNGTON E.M.H.,
- LOVELAND P.J., 1996. Magnetic susceptibility of soil: An Evaluation of Conflicting Theories using a national data set, Geophys J Int;127:728-734.
- LECOANET H., LÉVESQUE F., SEGUNA S., 1999. Magnetic susceptibility in environmental applications: comparison of field probes. Phys. Earth Planet. Inter. 115, 191 – 204.
- MULLINS C.E., TITE M.S., 1973. Magnetic viscosity, quadrature susceptibility and frequency dependence of susceptibility in single–domain assemblages of magnetite and maghaemite. J. Geophys. Res. 78, 804-809.
- STEFANIE A. BRACHFELD., 2006. High-field magnetic susceptibility (χHF) as a proxy of biogenic sedimentation along the Antarctic Peninsula, Physics of The Earth and Planetary Interiors , 156, 274-282.
Details
| Other ID | JA25RH22VT |
|---|---|
| Journal Section | Articles |
| Authors | |
| Publication Date | July 13, 2016 |
| Published in Issue | Year 2008 Volume: 7 Issue: 1 |