Microfacies analysis and depositional environment reconstruction of the Qom Formation, Sirjan area, southwest of the Kerman [PDF]
برونزدهای سازند قم در ناحیه سیرجان (جنوب غربی کرمان، حوضه پیش کمان سنندج-سیرجان) با 156 متر ضخامت، عمدتاً متشکل از سنگ آهکهای متوسط تا ضخیم لایه و تودهای و مارن میباشد.
Mohammad Dastanpour +2 more
doaj +3 more sources
Minimal Symptoms From a 7-Month Retained Guidewire Following Acute Non-Tunneled Hemodialysis Catheter Insertion: A Case Report. [PDF]
ABSTRACT Central venous catheterization (CVC), commonly used for hemodialysis due to its rapid access and immediate utility, carries risks—including the rare complication of guidewire retention. While typically identified early, retained guidewires can occasionally go unnoticed and migrate, leading to delayed and unexpected symptoms.
Saghafi MS +3 more
europepmc +2 more sources
The role of fossils in the microfacies studies and recognizing the sequence boundaries of the Qom Formation: A case study in Ghasr-e-Bahram Section, northwest part of Siahkuh, south Garmsar [PDF]
Sequence stratigraphy is a branch of stratigraphy that can enable us to correlate deposits with considerable accuracy. This research aims to investigate the role of fossils in the recognition of system tracts and sequence boundaries along succession ...
Jahanbakhash Daneshian +1 more
doaj +1 more source
Single-Crystal-to-Single-Crystal Transformation in a Copper(II) Complex: Structural and Spectroscopic Insights into Methanol Elimination and Hydrogen Bond Network Formation. [PDF]
A methanol‐ligated copper(II) complex undergoes a single‐crystal‐to‐single‐crystal transformation upon solvent loss, retaining crystallinity while reorganizing its coordination geometry and hydrogen‐bonding network. This study investigates the single‐crystal‐to‐single‐crystal (SCSC) transformations of a copper(II) complex, [Cu(L1)2(acac)2]·2CH3OH (1 ...
Mirtamizdoust B +4 more
europepmc +2 more sources
Microfacies, sedimentary environmental model and relative sea level change of marly strata of the Qom Formation in Zarrin-Abad section, South of Zanjan [PDF]
In order to reconstruct the sedimentary environment of marly strata related to the upper parts of Qom Formation, one stratigraphic outcrop have been studied.
Javad Rabbani +2 more
doaj +1 more source
Biostratigraphy and Microfacies of Qom Formation in Urumieh – Dokhtar Zone, Iran [PDF]
In order to determine the accurate paleoenvironmental conditions of Qom Formation, one stratigraphic section was studied in the Urumieh-Dokhtar Zone (West of Ashtian). 60 thin sections of the Qom Formation, 71 m thick, were prepared and the distribution of benthic foraminifera was analyzed.
Zohreh Holakouee +3 more
openaire +3 more sources
Preliminary analysis of sedimentary characteristics and facies model of M-II layer in Kazakhstan Oilfield A [PDF]
The lithologic melange accumulation of areskum formation in akshabluk area is one of the key strata in exploration. Its basement inheritance controls the whole process of Jurassic sedimentation, and the filling and leveling gradually reduces the terrain ...
Pan Xuemei
doaj +1 more source
Public Health Implications of Latent Toxoplasmosis and Its Association With Type 2 Diabetes: A Case-Control Study in Qazvin, North-Western Iran. [PDF]
ABSTRACT Introduction Toxoplasma gondii is a worldwide‐distributed zoonotic parasite, causing latent infections in humans. Increasing evidence has suggested a possible link between toxoplasmosis and diabetes mellitus (DM), though data from Iran are limited. This study was conducted to determine the seroprevalence of latent T.
Modarresnia L +11 more
europepmc +2 more sources
Global regression evidence in the Middle Miocene strata in the Zanjan area [PDF]
The study of the effect of global regression on the Middle Miocene (upper parts of the Qom Formation and Lower parts of the Upper Red Formation) strata has been carried out on two stratigraphic sections in the Zanjan area, northwest Iran.
Javad Rabbani, Afshin Zohdi
doaj +1 more source
Tozlou Pb-Zn mineralization, ~250-300m long, and ~50m thick, is hosted by limestone units of the Qom Formation. The main mineralization zone occurred as vein-veinlets and vug infill textures, where mineralization is observed as Pb-Zn-bearing barite veins
Hamed Daneshvar +3 more
doaj +1 more source

