Reef building and carbonate production modes in the west-central Tethys during the Cenozoic
Changing components, rock textures, lithofacies, platform types and architecture throughout
time are unique characteristics of carbonate rocks. Characterizing these attributes has been …
time are unique characteristics of carbonate rocks. Characterizing these attributes has been …
Palaeocene to Miocene southern Tethyan carbonate factories: A meta‐analysis of the successions of South‐western and Western Central Asia
One hundred and forty‐four published successions of shallow‐water carbonates, deposited
between the Palaeocene and the Miocene, from the Levant to the Himalayas, have been re …
between the Palaeocene and the Miocene, from the Levant to the Himalayas, have been re …
[HTML][HTML] The Tethyan Seaway during the early to middle Miocene–New data and a review
Abstract The Tethyan Seaway was the connection between the Eastern and Western Tethys
which became restricted and finally closed during the Early and Middle Miocene. The …
which became restricted and finally closed during the Early and Middle Miocene. The …
Control of climate, sea-level fluctuations and tectonics on the pervasive dolomitization and porosity evolution of the Oligo-Miocene Asmari Formation (Dezful …
The Asmari reservoir properties in various hydrocarbon fields across the Dezful Embayment
(SW Iran) are modified by dolomitization. Petrographic and geochemical analyses of the …
(SW Iran) are modified by dolomitization. Petrographic and geochemical analyses of the …
Open fracture clustering: Integrating subsurface and outcrop analogues, Asmari Formation, SW Iran
Fracture networks play a significant role in controlling fluid flow in carbonate reservoirs. Here
we have utilized a modern and rigorous technique known as normalized correlation count …
we have utilized a modern and rigorous technique known as normalized correlation count …
The effects of diagenesis on the petrophysical and geochemical attributes of the Asmari Formation, Marun oil field, southwest Iran
The distribution of good reservoir quality and its causes is the main challenges in carbonate
reservoir characterization. This study investigates the effects of diagenetic processes on the …
reservoir characterization. This study investigates the effects of diagenetic processes on the …
Oligo-Miocene carbonate platform evolution in the northern margin of the Asmari intra-shelf basin, SW Iran
MA Dill, H Vaziri-Moghaddam, A Seyrafian… - Marine and petroleum …, 2018 - Elsevier
This study is based on seven outcrops along a regional transect in the central subdivision of
the Zagros Foreland Basin. This NE-SW trending transect extends for 140 km and covers the …
the Zagros Foreland Basin. This NE-SW trending transect extends for 140 km and covers the …
Sedimentological and diagenetic impacts on porosity systems and reservoir heterogeneities of the Oligo-Miocene mixed siliciclastic and carbonate Asmari reservoir in …
E Khazaie, Y Noorian, M Kavianpour… - Journal of Petroleum …, 2022 - Elsevier
Abstract The Asmari Formation is largely affected by some diagenetic processes such as
dolomitization, fracturing, and dissolution in the Mansuri oilfield. These features have …
dolomitization, fracturing, and dissolution in the Mansuri oilfield. These features have …
Carbonate platform evolution of the Asmari Formation in the east of Dezful Embayment, Zagros Basin, SW Iran
In this study, based on a multidisciplinary approach (biostratigraphy, cyclostratigraphy, and
facies analysis), the Asmari carbonate successions were evaluated across two platform-to …
facies analysis), the Asmari carbonate successions were evaluated across two platform-to …
Foraminiferal biofacies and depositional environments of the Burdigalian mixed carbonate and siliciclastic Dam Formation, Al-Lidam area, Eastern Province of Saudi …
Four outcrops along a west to east transect in the Al Lidam escarpment of Saudi Arabia were
investigated to understand the vertical and lateral distribution of foraminiferal assemblages …
investigated to understand the vertical and lateral distribution of foraminiferal assemblages …