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asbestiform

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Journal Article
Published: 01 November 2003
American Mineralogist (2003) 88 (11-12): 1970–1978.
.... Minerals with the former values would be classified as richterite and those with the latter as winchite. Regulatory agencies classify certain species of amphibole as asbestos when they occur in the asbestiform habit. These regulated species are riebeckite, cummingtonite-grunerite, anthophyllite...
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Journal Article
Published: 01 September 2024
American Mineralogist (2024) 109 (9): 1499–1512.
... or hydrothermal alteration of volcanic rocks. The particular erionite “species” is based on the dominant extra-framework cation, erionite-Ca, erionite-K, or erionite Na. Irrespective of the species, erionite can display a fibrous/asbestiform morphology and has been linked with cases of malignant mesothelioma...
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Journal Article
Published: 20 February 2020
Environmental & Engineering Geoscience (2020) 26 (1): 39–46.
...Elena Belluso; Alain Baronnet; Silvana Capella ABSTRACT The natural occurrence of asbestos (NOA) in rocks and soil has been known for many years in several areas of the world, differently from the natural presence of asbestiform minerals. In Italy, the mapping of NOA is mandatory according...
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Journal Article
Published: 20 February 2020
Environmental & Engineering Geoscience (2020) 26 (1): 21–28.
...R. Mark Bailey ABSTRACT The San Francisco Bay Area is underlain by bedrock of the Franciscan Assemblage, which outcrops in numerous places. A significant portion of these outcrops consists of rock types that contain both regulated and unregulated asbestiform minerals, including ultra-mafic...
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Journal Article
Published: 01 April 2019
Mineralogical Magazine (2019) 83 (2): 209–222.
...Roberto Giustetto; Loredana Macaluso; Gloria Berlier; Yadolah Ganjkhanlou; Luca Barale Abstract An unusual occurrence of asbestiform sepiolite, filling veins in the antigorite serpentinites of the Voltri Unit exposed in a borrow pit (now reclaimed) in the Deiva forest, near Sassello, NW Italy...
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Journal Article
Published: 01 November 2015
The Canadian Mineralogist (2015) 53 (6): 1049–1060.
...). Talc occurs as a fine-grained mass in anthophyllite fractures, between acicular anthophyllite partings, and as pseudomorphs after anthophyllite, with some occurring with an asbestiform habit. Thus, the talc alterations occur both parallel and perpendicular to the elongate anthophyllite, with the latter...
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Journal Article
Published: 01 August 2014
Mineralogical Magazine (2014) 78 (4): 919–940.
...R. Giustetto; K. Seenivasan; E. Belluso Abstract An atypical asbestiform sepiolite occurrence with exceptionally long fibres wrapped by a sheath of aliphatic hydrocarbons was found in the Gressoney Valley (Italian Western Alps) while monitoring asbestos presence in outcrops of serpentinite rocks...
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Journal Article
Published: 01 August 2011
American Mineralogist (2011) 96 (8-9): 1414–1417.
...Mickey E. Gunter; M. Darby Dyar; Antonio Lanzirotti; Jonathan M. Tucker; Elly A. Speicher Abstract We obtained oriented Fe-XANES spectra on three amphibole bundles of fiber (i.e., asbestiform morphology), two single-crystal fragments (i.e., nonasbestiform morphology), and one aggregate of thousands...
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Journal Article
Published: 01 August 2010
European Journal of Mineralogy (2010) 22 (4): 525–533.
...John D. Fitz Gerald; Richard A. Eggleton; John L. Keeling Abstract Asbestiform antigorite from Rowland Flat near Adelaide in South Australia is shown by scanning and transmission electron microscopy to consist of bundles of [010] fibres. Defects combine with grain boundaries to define flattened...
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Journal Article
Published: 01 December 2000
South African Journal of Geology (2000) 103 (3-4): 163–174.
...J. Gutzmer; Nicolas J. Beukes Abstract Asbestiform manjiroite and todorokite occur as infill of bedding parallel extension veinlets in supergene altered braunite-kutnahorite lutite at the Smartt Mine in the Kalahari manganese field, South Africa. Geological evidence and preliminary geochronological...
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Journal Article
Published: 01 December 1995
American Mineralogist (1995) 80 (11-12): 1093–1103.
Journal Article
Published: 01 August 1985
American Mineralogist (1985) 70 (7-8): 767–772.
...Roberto Compagnoni; Giovanni Ferraris; Marcello Mellini Abstract Carlosturanite is a new rock-forming silicate occurring in a network of veins crosscutting the antigorite serpentinite of Sampeyre in the Monviso ophiolite, Italy. It is light-brown, asbestiform, and the [010] fibers are paralleled...
Journal Article
Journal: GSA Bulletin
Published: 01 January 1905
GSA Bulletin (1905) 16 (1): 131–136.
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Italian regions and mineral species of naturally occurring non-asbestos classified asbestiform minerals (NONA) in rocks: asbestiform antigorite, asbestiform Ca-erionite with Ca-levyne, asbestiform F-edenite, asbestiform gedrite, asbestiform Mg-horneblende, asbestiform offretite, asbestiform polygonal serpentine, and asbestiform sepiolite. For the Aosta Valley and Piedmont regions, details are in the text.
Published: 20 February 2020
Figure 2. Italian regions and mineral species of naturally occurring non-asbestos classified asbestiform minerals (NONA) in rocks: asbestiform antigorite, asbestiform Ca-erionite with Ca-levyne, asbestiform F-edenite, asbestiform gedrite, asbestiform Mg-horneblende, asbestiform offretite
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Transmission electron microscopic image of cross section of an asbestiform composite made of axially textured intergrown fibrils of asbestiform antigorite (atg) with minor asbestiform polygonal serpentine (PS) and chrysotile (chrys).
Published: 20 February 2020
Figure 4. Transmission electron microscopic image of cross section of an asbestiform composite made of axially textured intergrown fibrils of asbestiform antigorite (atg) with minor asbestiform polygonal serpentine (PS) and chrysotile (chrys).
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FEG-SEM images of the GD4a erionite sample showing the asbestiform crystal habit. (a) Low-magnification picture; (b) high-magnification image of the previous fiber bundle.
Published: 01 September 2024
Figure 4. FEG-SEM images of the GD4a erionite sample showing the asbestiform crystal habit. ( a ) Low-magnification picture; ( b ) high-magnification image of the previous fiber bundle.
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Macroscopic similarity of mineral fiber bundle. (A) Vein filled with asbestiform antigorite (indicated by the yellow arrow). (B) Fibrous bundles of asbestiform antigorite. (C) Fibrous bundles of chrysotile.
Published: 20 February 2020
Figure 3. Macroscopic similarity of mineral fiber bundle. (A) Vein filled with asbestiform antigorite (indicated by the yellow arrow). (B) Fibrous bundles of asbestiform antigorite. (C) Fibrous bundles of chrysotile.
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SEM back-scattered electron images. (A) Asbestiform tremolite. (B) Chrysotile fiber bundles. (C) Abundant lamellar, pseudo-fibrous antigorite fragments. (D) Organic fiber.
Published: 20 February 2020
Figure 3. SEM back-scattered electron images. (A) Asbestiform tremolite. (B) Chrysotile fiber bundles. (C) Abundant lamellar, pseudo-fibrous antigorite fragments. (D) Organic fiber.
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Geological sketch map of natural occurrences of fibrous-asbestiform minerals in New Caledonia. The three major sites of nickel-mining activity are magnified (modified after DIMENC-SGNC, 2010). Sampling sites are indicated with a square.
Published: 20 February 2020
Figure 1. Geological sketch map of natural occurrences of fibrous-asbestiform minerals in New Caledonia. The three major sites of nickel-mining activity are magnified (modified after DIMENC-SGNC, 2010). Sampling sites are indicated with a square.
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Published: 20 February 2020
Table 1. List of naturally occurring non-asbestos classified asbestiform minerals (NONA) in decreasing order of finding frequency, detected in Piedmont and Aosta Valley regions, northwestern Alps, Italy, and the ideal chemical formula.