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akaturk Akademik ölçüm

Makale detayı · 2004

Complete Tertiary exhumation history of the Menderes massif western Turkey an alternative working hypothesis

Dergi

Terra Nova

ISSN 0954-4879

YÖKSİS OpenAlex SJR Q1 JCR Q1 Atıf 132 Üst %10 Yüzdelik 90.7% FWCI 3.3
Yıl
2004
Tür
article

Veri kaynağı ayrımı

  • YÖKSİS YÖKSİS makale kaydı
  • YÖKSİS dergi adı Terra Nova
  • Katalog eşleşmesi (ISSN) Terra Nova
  • OpenAlex OpenAlex zenginleştirmesi (özet, atıf, konular)

Özet

OpenAlex · İngilizce

Abstract The main exhumation of the Menderes massif, western Turkey, occurred along an originally N‐dipping Datça–Kale main breakaway fault that controlled depositions in the Kale and the Gökova basins during the Oligocene – Early Miocene interval. The isostatically controlled upward bending of the main breakaway fault brings the lower plate rocks to the surface. In the Early Miocene, E–W‐trending N‐ and S‐dipping graben‐bounding faults fragmented the exhumed, dome‐shaped massif. The development of half grabens by rolling master fault hinges has allowed further exhumation of the central Menderes massif. After the Pliocene, high‐angle normal faults cut all of the previous structures. This model suggests that the Menderes massif is a single large metamorphic core complex that has experienced a two‐stage exhumation process.

Konular

Atıflar

OpenAlex cited_by_count. WoS veya Scopus atıf sayısı değildir; o kaynaklar için ayrı kolon yoktur.

132 atıf

OpenAlex cited_by_count (önbellek / veritabanı)

Yazarlar

  1. GÜROL SEYİTOĞLU
  2. VEYSEL IŞIK ANKARA ÜNİVERSİTESİ
  3. Ibrahim Cemen