saponite


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Related to saponite: Nontronite

sap·o·nite

 (săp′ə-nīt′)
n.
A clay mineral that is a hydrous silicate of aluminum and magnesium and occurs in soft amorphous masses in the cavities of certain rocks.

[Latin sāpō, sāpōn-, hair dye; see saponin + -ite.]

saponite

(ˈsæpəˌnaɪt)
n
(Minerals) a clay mineral consisting of hydrated magnesium aluminium silicate and occurring in metamorphic rocks such as serpentine
[C19: from Swedish saponit (a rendering of German Seifenstein soapstone), from Latin sāpō soap]

sap•o•nite

(ˈsæp əˌnaɪt)

n.
a clay mineral, hydrous magnesium aluminum silicate, belonging to the montmorillonite group: found as a soft filling in rock cavities.
[1840–50; < Swedish saponit < Latin sāpō soap]
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References in periodicals archive ?
Pozas, Textural and structural modifications of saponite from Cerro del Aquill by acid treatment, Clay Minerals, 36, 483 (2001).
Location of works, place of delivery supplies or performance: path of Saponite 61200 ARGENTAN
Smectite clays such as montmorillonite, hectorite, and saponite have been used as inorganic fillers in many polymers.
To distinguish montmorillonite from nantronite, saponite, and beidellite Li saturation and heat treatment was used (Moore and Reynolds, 1989).
2003) record saponite as the main phyllosilicate in the contact between the marl-limestone rhythmite and doleritic laccolith of Sierra de Priego (Cordoba), as a consequence of a late hydrothermal process after contact metamorphism produced by the intrusion of subvolcanic rocks.
The uncured composition of claim 1, wherein the layered filler comprises at least one silicate selected from montmorillonite, nontronite, beidellite, bentonite, volkonskoite, laponite, hectorite, saponite, sauconite, magadite, kenyaite, stevensite, vermiculite, halloysite, aluminate oxides, hydrotalcite and mixtures thereof.
Le seul changement architectural important coincide avec l'arrivee du peuple du Dorset tardif ayant mis en valeur des couloirs triangulaires distinctifs et des supports a lampes en saponite.
Moreover, the study explains that talc is present in close proximity to the carbonate locations - rather than previously suggested saponite - and talc-carbonate alteration of high-Mg precursor rocks has taken place.
Among the new entries are aluminum hydroxide adjuvant, disodium edetate, ethyl lactate, hectorite, lactose spray dried, lauric acid, linoleic acid, raffinose, and saponite.
Saponite, a member of the smectite group, has been identified at the Canadian Museum of Nature as dull, opaque, beige, spherical aggregates in cavities in a Francon quarry dike.