INVESTIGATING OF RELATIVE CRUSTAL THICKNESSES VARIATION OF CRETAN REGION WITH MAGNETIC AND FREE AIR GRAVITY ANOMALIES

Volume: 11 Number: 1 January 1, 2009
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INVESTIGATING OF RELATIVE CRUSTAL THICKNESSES VARIATION OF CRETAN REGION WITH MAGNETIC AND FREE AIR GRAVITY ANOMALIES

Abstract

Cretan Arc area where the plates of Africa and Aegean converge, is an active subduction still undergoing. In this respect the Cretan Arc is one of the most complex within the Eastern Mediterranean tectonics. In order to explain this structure, the crustal structure of this area lying in the coordinates 230 00ı -280 00ı east longitudes and 330 00ı -360 40ı north latitudes was tried to be investigated with free-air gravity and magnetic anomalies. There is a reciprocal relationship between the anomalies for determining crustal thicknesses. Therefore this approach can give general information about relative crustal thicknesses. The crustal thickness are thicker in the south of the Island of Crete compared with its north and accordingly the crustal thickness get relatively thinner toward the inward of the Aegean Sea observed from the both gravity and magnetic anomalies.

Keywords

References

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Details

Primary Language

Turkish

Subjects

-

Journal Section

-

Authors

Tolga Gönenç This is me
Türkiye

Publication Date

January 1, 2009

Submission Date

January 1, 2009

Acceptance Date

-

Published in Issue

Year 2009 Volume: 11 Number: 1

APA
Gönenç, T., Akgün, M., & Ergün, M. (2009). GİRİT BÖLGESİNİN İZAFİ KABUK KALINLIĞI DEĞİŞİMİNİN MANYETİK VE SERBEST HAVA GRAVİTE ANOMALİLERİ İLE İRDELENMESİ. Dokuz Eylül Üniversitesi Mühendislik Fakültesi Fen Ve Mühendislik Dergisi, 11(1), 44-56. https://izlik.org/JA24PZ49XZ
AMA
1.Gönenç T, Akgün M, Ergün M. GİRİT BÖLGESİNİN İZAFİ KABUK KALINLIĞI DEĞİŞİMİNİN MANYETİK VE SERBEST HAVA GRAVİTE ANOMALİLERİ İLE İRDELENMESİ. DEUFMD. 2009;11(1):44-56. https://izlik.org/JA24PZ49XZ
Chicago
Gönenç, Tolga, Mustafa Akgün, and Mustafa Ergün. 2009. “GİRİT BÖLGESİNİN İZAFİ KABUK KALINLIĞI DEĞİŞİMİNİN MANYETİK VE SERBEST HAVA GRAVİTE ANOMALİLERİ İLE İRDELENMESİ”. Dokuz Eylül Üniversitesi Mühendislik Fakültesi Fen Ve Mühendislik Dergisi 11 (1): 44-56. https://izlik.org/JA24PZ49XZ.
EndNote
Gönenç T, Akgün M, Ergün M (January 1, 2009) GİRİT BÖLGESİNİN İZAFİ KABUK KALINLIĞI DEĞİŞİMİNİN MANYETİK VE SERBEST HAVA GRAVİTE ANOMALİLERİ İLE İRDELENMESİ. Dokuz Eylül Üniversitesi Mühendislik Fakültesi Fen ve Mühendislik Dergisi 11 1 44–56.
IEEE
[1]T. Gönenç, M. Akgün, and M. Ergün, “GİRİT BÖLGESİNİN İZAFİ KABUK KALINLIĞI DEĞİŞİMİNİN MANYETİK VE SERBEST HAVA GRAVİTE ANOMALİLERİ İLE İRDELENMESİ”, DEUFMD, vol. 11, no. 1, pp. 44–56, Jan. 2009, [Online]. Available: https://izlik.org/JA24PZ49XZ
ISNAD
Gönenç, Tolga - Akgün, Mustafa - Ergün, Mustafa. “GİRİT BÖLGESİNİN İZAFİ KABUK KALINLIĞI DEĞİŞİMİNİN MANYETİK VE SERBEST HAVA GRAVİTE ANOMALİLERİ İLE İRDELENMESİ”. Dokuz Eylül Üniversitesi Mühendislik Fakültesi Fen ve Mühendislik Dergisi 11/1 (January 1, 2009): 44-56. https://izlik.org/JA24PZ49XZ.
JAMA
1.Gönenç T, Akgün M, Ergün M. GİRİT BÖLGESİNİN İZAFİ KABUK KALINLIĞI DEĞİŞİMİNİN MANYETİK VE SERBEST HAVA GRAVİTE ANOMALİLERİ İLE İRDELENMESİ. DEUFMD. 2009;11:44–56.
MLA
Gönenç, Tolga, et al. “GİRİT BÖLGESİNİN İZAFİ KABUK KALINLIĞI DEĞİŞİMİNİN MANYETİK VE SERBEST HAVA GRAVİTE ANOMALİLERİ İLE İRDELENMESİ”. Dokuz Eylül Üniversitesi Mühendislik Fakültesi Fen Ve Mühendislik Dergisi, vol. 11, no. 1, Jan. 2009, pp. 44-56, https://izlik.org/JA24PZ49XZ.
Vancouver
1.Tolga Gönenç, Mustafa Akgün, Mustafa Ergün. GİRİT BÖLGESİNİN İZAFİ KABUK KALINLIĞI DEĞİŞİMİNİN MANYETİK VE SERBEST HAVA GRAVİTE ANOMALİLERİ İLE İRDELENMESİ. DEUFMD [Internet]. 2009 Jan. 1;11(1):44-56. Available from: https://izlik.org/JA24PZ49XZ

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