TY  - JOUR
T1  - Progressive Britle-Ductile Deformation DM the Demirköy Pluton of the Strandjha Massive of Thrace-Turkey
AU  - Çağlayan, M-atilla
AU  - Şengün, Metin
AU  - Yurtsever, Ayhan
PY  - 1990
DA  - March
JF  - Bulletin  of the Mineral Research and Exploration
JO  - Bull.Min.Res.Exp.
PB  - Maden Tetkik ve Arama Genel Müdürlüğü
WT  - DergiPark
SN  - 0026-4563
SP  - 77
EP  - 87
VL  - 110
IS  - 110
LA  - en
AB  - Demirköy pluton, a Lower Cretaceous granitic body of the Strandjha massive of Thrace-Turkey, vary compositionallyfrom a syeno-granite to quartz-diorite. The periphery of the granite has been converted to mortar gneiss and mylonitegneiss/schist. The host rocks, where they are of a pelitic origin, have been transformed into foliated contact schists comprisingcordierite and andalusite. The intensity of shear shows a progressive diminution avvay from the periphery. The brittle-ductiledeformation is ascribed to the emplacement of the granite causing multistage developments of multidirectional cleavage, kingtype folding and shear pods that are observable in macroscopic and microscopic dimensions. The deformation is not attributed tolarge displacements, but is rather interpreted as the cumulative result of en echelon shearing.
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UR  - https://dergipark.org.tr/tr/pub/bulletinofmre/issue//52275
L1  - https://dergipark.org.tr/tr/download/article-file/44581
ER  -