Callovian-Oxfordian sedimentary microfacies in the middle of Block on the right bank of the Amu Darya Basin, Turkmenistan

[1]  M. Ader,et al.  Microfacies, diagenesis and hydrocarbon potential of the Neoproterozoic cap carbonate of the southern Amazon Craton , 2020 .

[2]  B. Nabawy,et al.  Implementation of sedimentary facies and diagenesis on the reservoir quality of the Aquitanian‐Burdigalian Rudeis Formation in the Gulf of Suez, Egypt: A comparative surface and subsurface study , 2019, Geological Journal.

[3]  Ting Zhang,et al.  Characteristics and controlling factors of the Lower–Middle Jurassic sandstone reservoirs in Amu Darya right bank area, Turkmenistan , 2019, Arabian Journal of Geosciences.

[4]  Mu-wei Cheng,et al.  High-resolution sequence divisions and stratigraphic models of the Amu Darya right bank , 2019, Arabian Journal of Geosciences.

[5]  A. Husinec,et al.  Relative Sea-Level Changes Recorded on an Isolated Carbonate Platform: Tithonian to Cenomanian Succession, Southern Croatia , 2006 .

[6]  G. Dromart,et al.  Jurassic evolution of the Arabian carbonate platform edge in the central Oman Mountains , 2005, Journal of the Geological Society.

[7]  U. Krähenbühl,et al.  Combined osmium and strontium isotopic study of the Cretaceous-Tertiary boundary at Sumbar, Turkmenistan: A test for an impact vs. a volcanic hypothesis , 1995 .

[8]  C. Ravenne,et al.  Systems tracts and depositional sequences in a carbonate setting: a study of continuous outcrops from platform to basin at the scale of seismic lines , 1991 .

[9]  Róbert,et al.  Unique signature of carbonate strata and the development of depositional sequence and systems tract models for ramps, rimmed shelves, and detached platforms , 1991 .