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Farid Moore

Researcher at Shiraz University

Publications -  190
Citations -  8078

Farid Moore is an academic researcher from Shiraz University. The author has contributed to research in topics: Microplastics & Biology. The author has an hindex of 45, co-authored 173 publications receiving 5680 citations. Previous affiliations of Farid Moore include Shiraz University of Medical Sciences & King's College London.

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Hydrogeochemical and ecological risk assessments of trace elements in the coastal surface water of the southern Caspian Sea

TL;DR: In this article, the occurrence, distribution, and potential ecological risk of trace elements along with the hydrogeochemical characteristics of coastal surface water collected from the southern Caspian coasts in the Mazandaran province of Iran were investigated.

Potentially Toxic Elements Contamination in Sediment, Surface and Pore water of Maharlu Saline Lake, South - West Iran

TL;DR: In this paper, a study aimed at assessing potentially toxic elements (PTEs) distribution in sediment, surface and pore water samples of Maharlu Lake was presented, where the samples were collected from each compartment and the total concentration of PTEs (Al, Fe, Sc, Cr, Co, Ni, Zn, As, Mn, Fe and Cd) analyzed by inductively coupled plasma optical emission spectrometry (ICP-OES).
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Leached caps mineralogy and geochemistry as supergene enrichment fertility indicators, Meiduk and Parkam porphyry copper deposits, SW Iran

TL;DR: In this paper, the fertility of supergene enrichment zones may be inferred from the mineralogical and geochemical characteristics of associated leached caps in Meiduk and Parkam porphyry copper deposits.
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Microplastics (MPs) distribution in surface sediments of the Freidounkenar paddy Wetland.

TL;DR: In this paper , the occurrence of microplastics in surface sediment of the Freidounkenar International Wetland (Northern Iran), a valuable habitat for migratory birds, was assessed.

Hydrothermal garnet in porphyry copper related skarn deposits, Ali-Abad, Yazd Province, Iran

TL;DR: The Ali-Abad porphyry copper deposit is located in the Central Iranian magmatic belt as mentioned in this paper, where the following mineral assemblage has occurred in the altered conglomerate: Garnet (andradite-grossular) + epidote+ quartz + calcite + pyrite Skarnification have only occurred in reactive carbonate clasts of the conglomerates.