Matches in SemOpenAlex for { <https://semopenalex.org/work/W2110406735> ?p ?o ?g. }
Showing items 1 to 79 of
79
with 100 items per page.
- W2110406735 endingPage "109" @default.
- W2110406735 startingPage "100" @default.
- W2110406735 abstract "Abstract The Tepearasi Formation of the autochthonous Geyikdagi Group in the Central Tauride Belt, SE of Beysehir, is Dogger in age and consists dominantly of massive limestones and greyish dolomites occurring within the middle to upper sections. The total thickness of the dolomitic levels ranges from 100–300 m and laterally extends 500–700 m. Three types of dolomite were distinguished through petrographic analyses: homogeneous, mottled (saddle-crystalline) and joint-filling dolomite, which were interpreted to have formed in two different stages, early diagenetic and late diagenetic. The homogeneous dolomite of the early diagenetic stage is light-coloured and monotonous-textured and shows the form of a dolosparite mosaic. The mottled dolomite formed in the late diagenetic stage is light- to dark-coloured and coarsely granular idiomorphic. The other type of late diagenetic dolomite, described as the joint-filling type, presents a crystal growth pattern from the joint walls towards the centre of the joint space. It is associated with coarse calcite crystals as well as primary dolomite crystal clasts which were formed in the early diagenetic stage. In addition to these characteristics, cataclastic texture indicating the influence of tectonism is also observed. Microtexture-oriented scanning electron microscopy (SEM) studies indicate that mottled dolomites show zonal structures and contain secondary dissolution vugs. SEM studies also revealed the existence of some remains (calcite, clay etc.) in joint-filling dolomites. Analyses by energy dispersive spectrometry (EDS) indicate the existence of clay minerals (likely to be illite) in the pores of dolomite. Isotope studies conducted to shed light onto the origin of the dolomites of the Tepearasi Formation yielded the results of δ18O=-2.48 to −3.87%‰ and δ13C=0.93 to 1.12%‰ for the early diagenetic homogeneous dolomites. Mottled and joint-filling type dolomites of the late diagenetic stage, on the other hand, gave the results of δ18O = −5.42 to −7.12%‰, and δ13C=-2.29 and −5.70 respectively. X-Ray diffractometry (XRD) and energy dispersive analysis X-Ray (EDAX), atomic absorption spectrometry (AAS) analyses, results of petrographic data, and δ18O and δ13C values suggest that the early diagenetic dolomitization in the Tepearasi Formation occurred under the control of hypersaline (rich in Mg) and fresh water mixing zone. The late diagenetic dolomites partly developed under the control of tectonic thrusting." @default.
- W2110406735 created "2016-06-24" @default.
- W2110406735 creator A5030410406 @default.
- W2110406735 creator A5048514477 @default.
- W2110406735 date "2010-09-07" @default.
- W2110406735 modified "2023-10-16" @default.
- W2110406735 title "Microtextural Characteristics and Origin of Dolomites in the Tepearasi Formation, SW of Beysehir-Konya, Turkey" @default.
- W2110406735 cites W1531383480 @default.
- W2110406735 cites W1971604371 @default.
- W2110406735 cites W1993105506 @default.
- W2110406735 cites W2006513617 @default.
- W2110406735 cites W2009188426 @default.
- W2110406735 cites W2032336958 @default.
- W2110406735 cites W2036680375 @default.
- W2110406735 cites W2053138706 @default.
- W2110406735 cites W2054172322 @default.
- W2110406735 cites W2054223043 @default.
- W2110406735 cites W2084146046 @default.
- W2110406735 cites W2121313833 @default.
- W2110406735 cites W2135874023 @default.
- W2110406735 cites W2139227477 @default.
- W2110406735 cites W2156033532 @default.
- W2110406735 cites W2159337285 @default.
- W2110406735 cites W2230958246 @default.
- W2110406735 cites W2517847674 @default.
- W2110406735 cites W4250980847 @default.
- W2110406735 doi "https://doi.org/10.1111/j.1755-6724.2002.tb00075.x" @default.
- W2110406735 hasPublicationYear "2010" @default.
- W2110406735 type Work @default.
- W2110406735 sameAs 2110406735 @default.
- W2110406735 citedByCount "0" @default.
- W2110406735 crossrefType "journal-article" @default.
- W2110406735 hasAuthorship W2110406735A5030410406 @default.
- W2110406735 hasAuthorship W2110406735A5048514477 @default.
- W2110406735 hasConcept C127313418 @default.
- W2110406735 hasConcept C130452526 @default.
- W2110406735 hasConcept C151730666 @default.
- W2110406735 hasConcept C164421858 @default.
- W2110406735 hasConcept C17409809 @default.
- W2110406735 hasConcept C175551986 @default.
- W2110406735 hasConcept C199289684 @default.
- W2110406735 hasConcept C2779429093 @default.
- W2110406735 hasConcept C2780181037 @default.
- W2110406735 hasConcept C2780191791 @default.
- W2110406735 hasConcept C40212044 @default.
- W2110406735 hasConcept C59235061 @default.
- W2110406735 hasConceptScore W2110406735C127313418 @default.
- W2110406735 hasConceptScore W2110406735C130452526 @default.
- W2110406735 hasConceptScore W2110406735C151730666 @default.
- W2110406735 hasConceptScore W2110406735C164421858 @default.
- W2110406735 hasConceptScore W2110406735C17409809 @default.
- W2110406735 hasConceptScore W2110406735C175551986 @default.
- W2110406735 hasConceptScore W2110406735C199289684 @default.
- W2110406735 hasConceptScore W2110406735C2779429093 @default.
- W2110406735 hasConceptScore W2110406735C2780181037 @default.
- W2110406735 hasConceptScore W2110406735C2780191791 @default.
- W2110406735 hasConceptScore W2110406735C40212044 @default.
- W2110406735 hasConceptScore W2110406735C59235061 @default.
- W2110406735 hasIssue "1" @default.
- W2110406735 hasLocation W21104067351 @default.
- W2110406735 hasOpenAccess W2110406735 @default.
- W2110406735 hasPrimaryLocation W21104067351 @default.
- W2110406735 hasRelatedWork W1861029346 @default.
- W2110406735 hasRelatedWork W2036361498 @default.
- W2110406735 hasRelatedWork W2110406735 @default.
- W2110406735 hasRelatedWork W2556674629 @default.
- W2110406735 hasRelatedWork W3136940746 @default.
- W2110406735 hasRelatedWork W3146497180 @default.
- W2110406735 hasRelatedWork W3146852307 @default.
- W2110406735 hasRelatedWork W4224941703 @default.
- W2110406735 hasRelatedWork W4230884620 @default.
- W2110406735 hasRelatedWork W4240302151 @default.
- W2110406735 hasVolume "76" @default.
- W2110406735 isParatext "false" @default.
- W2110406735 isRetracted "false" @default.
- W2110406735 magId "2110406735" @default.
- W2110406735 workType "article" @default.