Results 141 to 150 of about 3,998,312 (187)

Interface flexibility controls the nucleation and growth of supramolecular networks. [PDF]

Nat Chem
Caroprese V, Tekin C, Cencen V, Mosayebi M, Asmari N, Liverpool TB, Woolfson DN, Fantner GE, Bastings MMC.   +8 more
europepmc   +1 more source

Challenges and insights: Methamphetamine analysis in post-mortem putrefied human tissues in a hot climate. [PDF]

Saudi Pharm J
Alasmari A, Alhejaili A, Alharbi H, Alzahrani M, Zughaibi T.   +4 more
europepmc   +1 more source

Feasibility analysis on the application of the Maillard reaction in developing Lentinula edodes umami seasoning: Based on the umami substances, sensory quality, physicochemical properties of the products. [PDF]

Food Chem X
Qiu J, Li H, Zhang L, Li J, Fang Z, Li C, Chen H, Al-Asmari F, Sameeh MY, Wu W, Liu Y, Zeng Z.   +11 more
europepmc   +1 more source

A hermetically closed sample chamber enables time-lapse nano-characterization of pathogenic microorganisms in-vitro

Braun E, Andany SH, Kangül M, Asmari NS, McKinney JD, Fantner GE.   +5 more
europepmc   +1 more source

THE ORIGIN OF DOLOMITE IN THE ASMARI FORMATION (OLIGOCENE-LOWER MIOCENE), DEZFUL EMBAYMENT, SW IRAN

Journal of Petroleum Geology, 2006
Dolomitisation is an important factor controlling reservoir quality in the Asmari Formation in many producing fields in SW Iran. Dolostones have higher average porosities than limestones. Petrographic and geochemical studies have been used to determine the causes of Asmari dolomitisation at the Bibi Hakimeh and Marun fields and at the Khaviz anticline.
J A D Dickson
exaly   +4 more sources

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Paleoenvironmental model and sequence stratigraphy of the Asmari Formation in southwest Iran

Historical Biology, 2007
The Asmari Formation is a thick carbonate succession of the Oligo-Miocene in southwest Iran (Zagros Basin). The Zagros Basin was a continental margin attached to the eastern edge of Africa throughout the Phanerozoic. The foraminiferal limestone from the Asmari Formation has been studied to determine its microfacies, paleoenvironments and sedimentary ...
Hossein Vaziri-Moghaddam
exaly   +2 more sources

Control of climate, sea-level fluctuations and tectonics on the pervasive dolomitization and porosity evolution of the Oligo-Miocene Asmari Formation (Dezful Embayment, SW Iran)

Sedimentary Geology, 2022
The Asmari reservoir properties in various hydrocarbon fields across the Dezful Embayment (SW Iran) are modified by dolomitization. Petrographic and geochemical analyses of the dolomitized Asmari Formation units highlight their origin in the Bibi Hakimeh
Reza Moussavi-Harami, Asadollah Mahboubi
exaly   +2 more sources

Biostratigraphy and depositional environment evolution of the Asmari Formation at the Shajabil anticline, Iran

Arabian Journal of Geosciences, 2013
In the present research, biostratigraphy and paleoecology of the Asmari Formation at the Shajabil anticline, northwest Yasuj in the Izeh zone are discussed. The Asmari Formation at the studied area is Rupelian–Chattian to Burdigalian in age. In the study, 18 genera and 29 species of benthic foraminifera have been identified.
Zahra Saleh
exaly   +2 more sources

Integrated Rock Typing in Asmari Formation of Gachsaran Field

Proceedings, 2009
As part of an integrated reservoir modelling and simulation project, a rock-typing study has been performed on the carbonate Asmari Formation of Gachsaran Field (Iran). The current paper presents the challenges and results of integrating different disciplines in the definition of rock-types.
V. De Groen, M. Fuchs, S.M. Mirzadeh
openaire   +1 more source

STRONTIUM ISOTOPE STRATIGRAPHY OF THE ASMARI FORMATION (OLIGOCENE - LOWER MIOCENE), SW IRAN

Journal of Petroleum Geology, 2007
The Asmari Formation has been studied in the subsurface at the Bibi Hakimeh, Marun and Ahwaz oilfields and in an outcrop section from the Khaviz anticline. It consists of approximately 400 m of cyclic platform limestones and dolostones with subordinate intervals of sandstone and shale.
John McArthur, M F Thirlwall
exaly   +2 more sources