Results 31 to 40 of about 2,463 (203)

Non-occupational malignant pleural mesothelioma due to asbestos and non-asbestos fibres

open access: yesMonaldi Archives for Chest Disease, 2016
Background and aim. The occurrence of malignant pleural mesothelioma (MPM) has been reported among population groups with no documented professional exposure to asbestos fibres living in different geographic areas.
L. Proietti   +6 more
doaj   +1 more source

Metamorphic dolomitic marble-hosted talc from the Mulvoj area in the Western Pamir Mountains, Tajikistan

open access: yesMineralogia, 2023
Talc is crystallized in the metamorphic dolomitic rocks of the southwest Pamir mountains in the Mulvoj area, Tajikistan. Field studies show that talc is restricted to metamorphic dolomitic marble layers in the garnet-mica schist and gneiss.
Moazzen Mohssen   +2 more
doaj   +1 more source

Mineralogy, geochemistry and metamorphism of the early Proterozoic Vähäjoki iron ores, northern Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 1991
The Vähäjoki iron ores occupy the uppermost part of the Karelian (Early Proterozoic) quartzite-dolomite sequence deposited on the late Archaean basement in southern Lapland.
J. Liipo, K. Laajoki
doaj   +1 more source

Minerals of Pohorje marbles

open access: yesGeologija, 2013
In the Pohorje Mts, mostly outcrops of calcite marble can be found, which in places turn into dolomite marbles.The protolith carbonate rocks contained also detritical minerals, which remained unchanged or formed new mineralsduring metamorphosis. Minerals
Miha Jeršek   +4 more
doaj   +1 more source

Some mineralogical and geochemical aspects of chromium-bearing skarn minerals from northern Karelia, Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 1986
The chromiferous skarn mineral associations at Outokumpu have been described and a number of characteristic chromium-bearing minerals have been re-examined.
O. von Knorring, E. Condliffe, Y.L. Tong
doaj   +1 more source

Metastability of Tremolite at High Pressures and Temperatures [PDF]

open access: yes, 2020
Tremolite (Ca2Mg5Si8O22(OH)2), a hydrated calcium-bearing amphibole mineral, is a common constituent of subducting oceanic lithosphere and an important source of water for geological processes in subduction zones.
Ott, Jason Noel
core  

Kavokta Deposit, Middle Vitim Mountain Country, Russia: Composition and Genesis of Dolomite Type Nephrite

open access: yesGeosciences
The Kavokta deposit of the dolomite type nephrite is located in the Middle Vitim mountain country, Russia (Russian Federation). The deposit area is composed of granite of the Late Paleozoic Vitimkan complex.
Evgeniy V. Kislov
doaj   +1 more source

Characterization and Dielectric Study of Mihaliccik Tremolite

open access: yes, 2019
The natural tremolite Ca2Mg5Si8O22 OH 2 was obtained from Mihaliccik district of Eskisehir, Turkey 39.8787N 31.3806E . It is a part of the amphibole family of silicate minerals.
Ertugrul Izci
core   +1 more source

P–T Modelling Constrains the Depth of Emplacement of the Porto Azzurro Pluton and Implies Minor Exhumation Caused by the Zuccale Fault (Island of Elba, Italy)

open access: yesJournal of Metamorphic Geology, EarlyView.
ABSTRACT Understanding the pressure of emplacement of granitic intrusions is crucial to understanding the exhumation history of plutons and constraining the tectonic setting of magma emplacement. However, P–T and geochronological constraints from exhumed plutons are often characterized by large uncertainties, especially in shallow crustal settings with
Samuele Papeschi   +4 more
wiley   +1 more source

Tremolite Whitewashing and Pleural Calcifications

open access: yesChest, 1987
Radiologic screening of 688 inhabitants of the Metsovo area in Northwest Greece revealed that 323 (46.9 percent) had pleural calcifications. The percentage of positive examinations rose with age. Calcifications were observed in all four villages of the area where a material ("luto" soil) had been extensively used for whitewashing until 1940 to 1950. In
Constantopoulos, S. H.   +5 more
openaire   +3 more sources

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