BENTHIC FORAMINIFERAL BIOSTRATIGRAPHY OF MALATYA OLIGO-MIOCENE SUCCESSION (EASTERN TAURIDS, EASTERN TURKEY)
Journal Title: Bulletin of the Mineral Research and Exploration - Year 2015, Vol 150, Issue
Abstract
The benthic foraminiferal biostratigraphy of Oligo-Miocene aged Muratlı and Petekkaya formations which crop out over wide regions around Akçadağ town, west of Malatya pro- vince in Eastern Taurids were revealed in this study. Systematical sampling was carried out in measured stratigraphical sections in four locations in order to perform stratigraphical and paleontological investigations. Benthic foraminifera taken from 182 hard rock samples were defined and three biozones were determined as; SBZ 21-22, belonging to Oligocene (Rupe- lian - Early Chattian), SBZ 23 (Late Chattian) and SBZ 25 belonging to Lower Miocene in shallow marine deposits in the region. It was stated that the assemblage of planktic forami- nifer and nannoplankton which stratigraphically detected within Chattian - Burdigalian units in the succession most probably indicated Aquitanian age. Besides; Oligo-Miocene transition in the region was approved with this study based on biostratigraphical locations of benthic foraminiferal taxa.
LATE PERMIAN UNCONFORMITY AROUND ANKARA AND NEW AGE DATA ON THE BASEMENT ROCKS, ANKARA, TURKEY
At southwest of Gölbafl› (Ankara) there are two different sequences in tectonic contact. The one at the bottom with low-degree metamorphism is represented by phyllite, metabasite, crystallized limestone, schist and quart...
OSTRACOD FAUNA AND ENVIRONMENTAL FEATURES OF TERTIARY (PALEOGENENEOGENE) DEPOSITS IN YEDİKULE- İSTANBUL REGION
This study consists of micro paleontological assessments of samples taken from drills carried out around Yedikule area for the micro zonation study made by the Istanbul Municipality in European side of Istanbul province....
Geochemistry and tectonic signifi cance of the ophiolitic rocks of the Yarpuz-Kaypak (Amanoslar, Osmaniye) area
Yarpuz-Kaypak (Osmaniye) region, located in Amanos Mountains, contains harzburgitic tectonites and mafic cumulates. The tectonites are represented by serpantinized harzburgites, whereas the cumulates are characterized by...
BRIEF NOTE ON NEOGENE VOLCANISM in KEMALPAŞA–TORBALI BASIN (İZMİR)
This study was made in order to introduce Neogene volcanics the first time, which its presence has not been mentioned in previous investigations (Akdeniz et al., 1986; İnci, 1991; Kaya et al., 2007; Sözbilir et al., 2011...
AN APPROACH TO THE ORIGIN OF THE EARLY CAMBRIAN KARAÇAT IRON DEPOSIT (MANSURLU BASIN, ADANA) AND IRON DEPOSITS OUTCROPS AT ITS EASTERN PARTS
The Neoproterozoic basement and the Early Cambrian units are widely exposed around the Karaçat Iron Deposit and its surrounding, which are located at the eastern part of Tauride-Anatolide platform. The main mineralizatio...