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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Kenya (1)
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Nile River (1)
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North Africa
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Egypt
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Nubian Shield (1)
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Asia
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Japan
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Turkey
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Anatolia (79)
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East Anatolian Fault (6)
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Hatay Turkey (5)
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Istanbul Turkey (1)
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Lycian Taurus (6)
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Menderes Massif (9)
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Mammalia
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Rodentia
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Invertebrata
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Cypridocopina
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Trilobitomorpha
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Brachiopoda (1)
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Cnidaria
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Scleractinia (1)
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Echinodermata
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Mollusca
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Bivalvia (1)
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Cephalopoda
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Gastropoda (1)
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Porifera (1)
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Protista
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Foraminifera
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Fusulinina
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Fusulinidae (3)
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Rotaliina
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Globigerinacea
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Globigerinoides (1)
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Globorotaliidae
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Orbitoidacea
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Discocyclina (1)
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Orbitoididae (2)
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Rotaliacea
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Textulariina
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Plantae
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Mesozoic
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Cretaceous
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Upper Cretaceous
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Paleozoic
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Upper Carboniferous (3)
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Devonian (2)
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Lower Ordovician
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Upper Ordovician
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Permian
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Lower Permian
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Middle Permian (1)
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Upper Permian
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Permian-Triassic boundary (3)
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Silurian
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upper Paleozoic (1)
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Precambrian
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upper Precambrian
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Proterozoic
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igneous rocks
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metamorphic rocks
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minerals
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minerals (4)
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native elements
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rutile (1)
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pyroxene group
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orthopyroxene
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wollastonite group
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wollastonite (1)
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framework silicates
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feldspar group
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alkali feldspar
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K-feldspar (2)
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plagioclase (1)
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silica minerals
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quartz (1)
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zeolite group
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garnierite (1)
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orthosilicates
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garnet group
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grossular (1)
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kyanite (1)
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olivine group
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kirschsteinite (1)
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sillimanite (1)
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titanite group
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titanite (1)
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zircon group
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zircon (9)
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sorosilicates
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epidote group
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allanite (1)
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ring silicates
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tourmaline group (1)
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sheet silicates
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chlorite group
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clay minerals
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illite (4)
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mica group
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palygorskite (5)
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sepiolite (2)
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sulfates
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sulfides
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molybdenite (2)
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pyrite (1)
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wehrlite (1)
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Primary terms
-
absolute age (18)
-
Africa
-
East Africa
-
Kenya (1)
-
-
Nile River (1)
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North Africa
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Egypt
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Eastern Desert (1)
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Nile Delta (1)
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-
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Nubian Shield (1)
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Asia
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Arabian Peninsula
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Arabian Shield (1)
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Far East
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China
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Nanpanjiang Basin (1)
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Japan
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Kyushu (1)
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Indian Peninsula
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Afghanistan (1)
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India (1)
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Pakistan (1)
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Middle East
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Cyprus
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Troodos Massif (1)
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Dead Sea (1)
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Iran
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Elburz (1)
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Iraq (1)
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Israel (1)
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Syria (5)
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Turkey
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Amanos Mountains (5)
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Anatolia (79)
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Ankara Turkey (2)
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Antalya Turkey (18)
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East Anatolian Fault (6)
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Hatay Turkey (5)
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Istanbul Turkey (1)
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Konya Basin (2)
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Konya Turkey (7)
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Lycian Taurus (6)
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Menderes Massif (9)
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North Anatolian Fault (1)
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Pontic Mountains (3)
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Taurus Mountains (80)
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Turkish Aegean region (9)
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Tuz Golu (1)
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-
Zagros (4)
-
-
-
Atlantic Ocean
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North Atlantic (1)
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barite deposits (2)
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bauxite deposits (2)
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bibliography (1)
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biogeography (3)
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Canada
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Western Canada
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British Columbia
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Queen Charlotte Islands (2)
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carbon
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C-13/C-12 (5)
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C-14 (1)
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organic carbon (1)
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Cenozoic
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Bronze Age (1)
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Quaternary
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Holocene
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lower Holocene (1)
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upper Holocene
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Roman period (1)
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Pleistocene
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upper Pleistocene (2)
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upper Quaternary (3)
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Stone Age
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Paleolithic (1)
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Tertiary
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Neogene
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Miocene
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lower Miocene
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Aquitanian (1)
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middle Miocene
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Serravallian (1)
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upper Miocene
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Messinian (4)
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Pontian (1)
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Tortonian (3)
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-
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Pliocene
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lower Pliocene (1)
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-
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Paleogene
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Eocene
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middle Eocene
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Lutetian (1)
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upper Eocene (1)
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Oligocene
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lower Oligocene (1)
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middle Oligocene (1)
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Paleocene (2)
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upper Paleogene (1)
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upper Cenozoic (2)
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ceramic materials (1)
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Chordata
-
Vertebrata
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Rodentia
-
Myomorpha
-
Cricetidae (1)
-
-
-
-
-
-
-
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Producible fluid oil saturations of the Upper Cretaceous unconventional carbonate plays, northern Arabian plate
Characterization of palynological features of Cyclamen species native to Turkey and new approaches for their systematic significance
Comparative palynological survey of the species of Reseda L. (Resedaceae) from Turkey
Geochemical approach to the genesis of the Buyukkizilcik (Afsin) barite deposit, SE Turkey
Using an analytic hierarchy process-based index and geographic information system in geochemical exploration of gold
Benthic foraminifera from the Albian shallow-marine limestones in the Geyik Dağı area (Central Taurides), southern Turkey
Biostratigraphy and taxonomy of fusulinid foraminifera across the Upper Mississippian (upper Serpukhovian)–Lower Pennsylvanian (Bashkirian) successions from the Hadim Nappe, Central Taurides, southern Turkey
Fast Pliocene integration of the Central Anatolian Plateau drainage: Evidence, processes, and driving forces
Geological correlation between northern Cyprus and southern Anatolia
Paynita Permotaurica N. Gen., N. SP., and the Other Dagmaritin Foraminifera from the Changhsingian (Permian) of Southern Turkey: Review of Dagmaritin Phylogeny
Zoogeographical and stratigraphical distribution of the genus Zonocypris : Supportive evidence for Anatolian Diagonal and description of a new species from Turkey
Age and mantle sources of Quaternary basalts associated with “leaky” transform faults of the migrating Anatolia-Arabia-Africa triple junction
Cenozoic tectonic evolution of the Ecemiş fault zone and adjacent basins, central Anatolia, Turkey, during the transition from Arabia-Eurasia collision to escape tectonics
Phenacophragma Oezeri N. SP., a Benthic Foraminifera from Albian Shallow Marine Carbonates of the Geyİk Daği Area (Southern Turkey)
Late Triassic ostracods from the Lycian Nappes, southwestern Turkey: implications on taxonomy and palaeobiogeographical distribution
Carnian (Upper Triassic) Lavas and Tuffites from the Mersin Mélange: Evidence for Intraoceanic Arc Rifting in the Northern Neotethys
Abstract The Sivas Basin in central-eastern Anatolia is a north-verging salt-bearing fold-and-thrust belt including synorogenic salt tectonics. It formed between the northern leading edge of the Taurides platform and the Kırşehir block since Late Cretaceous time. We have constructed five regional cross-sections supported by field data and 2D seismic to constrain the structure of the basin and its evolution. The area is divided into three tectonic domains from south to north: (1) a Maastrichtian to Eocene north-verging fold-and-thrust belt, which terminates by a regional Eocene evaporitic level; (2) an Oligo-Miocene salt domain which contains two generations of minibasins separated by a salt canopy, forming a salt-and-thrust belt; and (3) a late Miocene to present day foreland basin. The cross-sections show the along-strike variations and the increasing shortening in the fold-and-thrust belt from west ( c. 15 km) to east ( c. 25 km). The thick salt allows for the intracutaneous propagation of the fold-and-thrust belt below a domain of salt withdrawal minibasins, decoupled as the initial salt thickness increases. In that case, the salt domain is thrusted both frontward and backward. Efficient exhumation followed by erosion of the fold-and-thrust resulted in synorogenic salt tectonics in the foreland and thus increased the mechanical resistance between them.
Chapter 23: Alteration, Mineralization, and Age Relationships at the Kışladağ Porphyry Gold Deposit, Turkey
Abstract The Miocene Kışladağ deposit (~17 Moz), located in western Anatolia, Turkey, is one of the few global examples of Au-only porphyry deposits. It occurs within the West Tethyan magmatic belt that can be divided into Cretaceous, Cu-dominant, subduction-related magmatic arc systems and the more widespread Au-rich Cenozoic magmatic belts. In western Anatolia, Miocene magmatism was postcollisional and was focused in extension-related volcanosedimentary basins that formed in response to slab roll back and a major north-south slab tear. Kışladağ formed within multiple monzonite porphyry stocks and dikes at the contact between Menderes massif metamorphic basement and volcanic rocks of the Beydağı stratovolcano in the Uşak-Güre basin. The mineralized magmatic-hydrothermal system formed rapidly (<400 kyr) between ~14.75 and 14.36 Ma in a shallow (<1 km) volcanic environment. Volcanism continued to at least 14.26 ± 0.09 Ma based on new age data from a latite lava flow at nearby Emiril Tepe. Intrusions 1 and 2 were the earliest (14.73 ± 0.05 and 14.76 ± 0.01 Ma, respectively) and best mineralized phases (average median grades of 0.64 and 0.51 g/t Au, respectively), whereas younger intrusions host progressively less Au (Intrusion 2A: 14.60 ± 0.06 Ma and 0.41 g/t Au; Intrusion 2 NW: 14.45 ± 0.08 Ma and 0.41 g/t Au; Intrusion 3: 14.39 ± 0.06 and 14.36 ± 0.13 Ma and 0.19 g/t Au). A new molybdenite age of 14.60 ± 0.07 Ma is within uncertainty of the previously published molybdenite age (14.49 ± 0.06 Ma), and supports field observations that the bulk of the mineralization formed prior to the emplacement of Intrusion 3. Intrusions 1 and 2 are altered to potassic (biotite-K-feldspar-quartz ± magnetite) and younger but deeper sodic-calcic (feldspar-amphibole-magnetite ± quartz ± carbonate) assemblages, both typically pervasive with disseminated to veinlet-hosted pyrite ± chalcopyrite ± molybdenite and localized quartz-feldspar stockwork veinlets and sodic-calcic breccias. Tourmaline-white mica-quartz-pyrite alteration surrounds the potassic core both within the intrusions and outboard in the volcanic rocks. Tourmaline was most strongly developed on the inner margins of the tourmaline-white mica zone, particularly along the Intrusion 1 volcanic contact where it formed breccias and veins, including Maricunga-style veinlets. Field relationships show that the early magmatic-hydrothermal events were cut by Intrusion 2A, which was then overprinted by Au-bearing argillic (kaolinite-pyrite ± quartz) alteration, followed by Intrusion 3 and late-stage, low-grade to barren argillic and advanced argillic alteration (quartz-pyrite ± alunite ± dickite ± pyrophyllite). Gold deportment changes with each successive hydrothermal event. The early potassic and sodic-calcic alteration controls much of the original Au distribution, with the Au dominantly deposited with feldspar and lesser quartz and pyrite. Tourmaline-white mica and argillic alteration events overprinted and altered the early Au-bearing feldspathic alteration and introduced additional Au that was dominantly associated with pyrite. Analogous Au-only deposits such as Maricunga, Chile, La Colosa, Colombia, and Biely Vrch, Slovakia, are characterized by similar alteration styles and Au deportment. The deportment of Au in these Au-only porphyry deposits differs markedly from that in Au-rich porphyry Cu deposits where Au is typically associated with Cu sulfides.