राखाडी किंवा हिरवे तंतुमय खनिज, व्यावसायिक एस्बेस्टोस हा एक महत्त्वाचा स्त्रोत आहे,

chrysotile's Usage Examples:

government would no longer oppose inclusion of chrysotile in the convention.

minerals of the serpentine subgroup, especially antigorite, lizardite, and chrysotile or white asbestos, all of which are commonly found in ultramafic rocks.

commercial asbestos types is broadly in the ratio 1:100:500 for chrysotile, amosite and crocidolite respectively.

in minerals as early as 1930, some minerals such as white asbestos (or chrysotile) and imogolite were actually shown to have a tubular structure.

Fibrous tremolite is sometimes found as a contaminant in vermiculite, chrysotile (itself a type of asbestos) and talc.

copper, iron, manganese, tin, coal, andalusite, chrysotile asbestos, kieselguhr, limestone, magnesite, talc and shale.

Minaçu is the seat of one of the world"s largest chrysotile asbestos mines.

to contain 25-40% asbestos, with amosite being the most common form of asbestos used, although a mixture of amosite and chrysotile was also common, and.

The most common asbestiform mineral is chrysotile, commonly called "white asbestos", a magnesium phyllosilicate part of.

Balangeroite is found in one of the most important chrysotile mines in Europe, the Balangero Serpentinite.

chrysotile of the serpentine class and those belonging to the amphibole class: amosite, crocidolite, tremolite, anthophyllite and actinolite.

The rock is composed of asbestos (chrysotile), an ultramafic rock.

are linked to chrysotile and asbestos exposure.