Late Palaeozoic–Cenozoic tectonic development of carbonate platform, margin and oceanic units in the Eastern Taurides, Turkey

2013 ◽  
Vol 372 (1) ◽  
pp. 167-218 ◽  
Author(s):  
A. H. F. Robertson ◽  
O. Parlak ◽  
Y. Metİn ◽  
Ö. Vergİlİ ◽  
K. Tasli ◽  
...  
Keyword(s):  
Carbonate Platform ◽  
Late Palaeozoic ◽  
Platform Margin ◽  
Tectonic Development ◽  
Carbonate Platform Margin

The Barremian-Aptian Evolution of The Eastern Arabian Carbonate Platform Margin (Northern Oman)

2003 ◽  
Vol 73 (5) ◽  
pp. 756-773 ◽  
Author(s):  
H. Hillgartner ◽  
F. S.P. van Buchem ◽  
F. Gaumet ◽  
P. Razin ◽  
B. Pittet ◽  
...  
Keyword(s):  
Carbonate Platform ◽  
Platform Margin ◽  
Carbonate Platform Margin

scholarly journals Cambrian Ordovician sedimentary facies and its evolution in Tadong area

2021 ◽  
Vol 329 ◽  
pp. 01055
Author(s):  
Ding Hansheng
Keyword(s):  
Oil And Gas ◽  
Carbonate Platform ◽  
Sedimentary Facies ◽  
Seismic Profile ◽  
Oil And Gas Exploration ◽  
Stratigraphic Framework ◽  
Lower Ordovician ◽  
Platform Margin ◽  
Carbonate Platform Margin ◽  
Order Sequence

In order to clarify the sedimentary development law under the Cambrian Ordovician regional stratigraphic framework in Tadong area, and lay a theoretical foundation for further oil and gas exploration in the study area. The distribution, characteristics and evolution of main sedimentary facies belts of Cambrian Ordovician are studied by means of drilling core observation, cast thin section identification, logging curve feature analysis, seismic profile and well connection profile. The results show that the Cambrian middle lower Ordovician in Tadong area is equivalent to a second-order sequence and can be further divided into 12 thirdorder sequences. Each third-order sequence is mainly composed of transgressive and highstand tracts. Carbonate platform margin beach facies and Reef (mound) beach complex facies are favorable reservoir development facies belts in this area; Under the regional stratigraphic framework, three types of sedimentary facies can be identified in Cambrian Ordovician, and a total of 10 subfacies are developed; The evolution of sedimentary facies is mainly controlled by the rise and fall of sea level, which is characterized by the migration of platform margin facies and the change of platform facies.

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