In a study of five chrysotile miners and millers with malignant pleural mesothelioma, Churg et al. (1984) noted a ratio of tremolite to chrysotile ranging from 3.9 to 12 (median 5.5). In a study of 83 shipyard workers and insulators with mesothelioma, Churg and Vedal (1994) found a geometric mean tremolite to chrysotile ratio of 12.8.
Tremolite is a calcic amphibole and the magnesian end-member of the tremolite – ferro-actinolite series, a continuous solid solution dictated by the substitution of Mg by Fe 2+.Tremolite was named in 1789 in reference to Tremola Valley (Switzerland) by Johann Georg Albrecht Höpfner, a Swiss journalist and pharmacist who investigated some …
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The quality of nephrite (jade) is directly related to the structural and compositional changes it undergoes during mineralization. This study is the first systematic analysis of the geochemical characteristics and composition changes of tremolite at various stages in the mineralization process of nephrite from Tieli, Heilongjiang, Northeastern …
Tremolite Meanings, Zodiacs, Planets, Elements, Colors, Chakras, and more. Science & Origin of TremoliteTremolite is composed of silicate minerals, the main being asbestos, and member of the amphibole group that crystallizes in the form of masses, fibrous aggregates, and prismatic crystals. It was named by Johann Georg Albrecht Höpfner in 1789 after the …
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Tremolite marble from Florence County, Wisconsin. Field of view 7 cm across. (Photo by Al Falster.) Tremolite is formed by the metamorphism of calcium-rich rocks such as limestone and dolostone. It occurs in numerous Precambrian rocks in the state, such as in Bad River dolomite (now metamorphosed to a marble) in Bayfield and Ashland Counties; in the …
This mineral was earlier (1782) called Säulenspath and Sternspath by Johann Ehrenreich von Fichtel for material from Sebeşu de Jos, Transylvania, Romania (for a full account of the early history of tremolite, see Roth, 2006). Type Locality: ⓘ Campolungo, Piumogna Valley, Leventina, Ticino, Switzerland. Tremolite forms a continuous series ...
2.2 x 1.2 x 0.6 cm. A terminated gem crystal of tremolite from Madagascar - rather rough on the surface but absolutely gemmy, with fine bottle-green color, through the interior. [Originally uploaded as diopside. An identical crystal has been analyzed by RRUFF (RRUFF Id. Tremolite X050169) by Raman spectroscope and was found to be a tremolite]
While the tremolite was in the HCl solution, any granular pieces of calcite or marble were located by the reaction trail of fizzing and removed from the sieve pan sitting in the acid bath. Once each batch had been submerged for 15 minutes it was removed from the acid bath and rinsed with fresh water for at least three rinses. Some batches were ...
amphiboles (Leake et al., 1997) tremolite forms part of the tremolite–actinolite–ferro-actinolite series: Whereas usually the dividing line between two species in a continuous solid solution series is set at the 50% point (Nickel and Grice, 1998), tremolite occupies only a narrow range. It is defined as having a
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Tremolite is one of the high vibration crystals, and resonates with a powerful energy. Its energy is felt within the highest chakras. This is particularly noticeable at both the third eye and crown chakra. Its energy is known to help you to open new pathways in the brain, allowing you to access the morphic field of knowledge.
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Sierra Leone: Cr-rich tremolite, deep green with Cr spectrum displayed. Comments. It is possible to misidentify tremolite, mistaking it for other amphiboles. Hexagonite is the rarest of the gem varieties of tremolite. If tremolite occurs in very tiny fibrous crystals, densely matted and interlocked, it is then known as nephrite (jade). Material ...
Hydration of mantle peridotites provides information on the exhumation history and on the fluid regime accompanying exhumation of these rocks (reservoirs involved, fluid/rock ratios, temperature of interaction). Highly depleted harzburgites and dunites of the Peridotite Nappe of New Caledonia are crosscut by fractures, which have been …