The Neotethyan ophiolites exposed in SE Anatolia–Syria occur along two,ENE-WSW-trending,sub-parallel belts(Fig.1).The ophiolites and ophiolitic mélanges in the southern belt include the Cretaceous K?z?lda?(Hatay),
We report here new geochemical and geochronological data from mafic-ultramafic rock suites in the Ankara Mé1ange in north-central Turkey, and present a new tectonic model for its origin. Considered as one of most...We report here new geochemical and geochronological data from mafic-ultramafic rock suites in the Ankara Mé1ange in north-central Turkey, and present a new tectonic model for its origin. Considered as one of most important relics of the Neotethyan realm in the region, the Ankara Mé1ange occurs between the Sakarya Continent （Eurasia） to the north and the Central Anatolian Crystalline Complex （CACC） to the south and includes remnants of the latest Triassic-early Jurassic Neotethyan oceanic lithosphere, fragments of Cretaceous seamounts,展开更多
文摘The Neotethyan ophiolites exposed in SE Anatolia–Syria occur along two,ENE-WSW-trending,sub-parallel belts(Fig.1).The ophiolites and ophiolitic mélanges in the southern belt include the Cretaceous K?z?lda?(Hatay),
基金supported by a grant from the General Directorate of Mineral Research and Exploration of Turkey (MTA, Ankara project no: 2007–2008.30.1601.d–f)
文摘We report here new geochemical and geochronological data from mafic-ultramafic rock suites in the Ankara Mé1ange in north-central Turkey, and present a new tectonic model for its origin. Considered as one of most important relics of the Neotethyan realm in the region, the Ankara Mé1ange occurs between the Sakarya Continent （Eurasia） to the north and the Central Anatolian Crystalline Complex （CACC） to the south and includes remnants of the latest Triassic-early Jurassic Neotethyan oceanic lithosphere, fragments of Cretaceous seamounts,
