The astrophyllite supergroup: nomenclature and classification. (1st February 2017)
- Record Type:
- Journal Article
- Title:
- The astrophyllite supergroup: nomenclature and classification. (1st February 2017)
- Main Title:
- The astrophyllite supergroup: nomenclature and classification
- Authors:
- Sokolova, Elena
Cámara, Fernando
Hawthorne, Frank
Ciriotti, Marco - Abstract:
- Here we report a nomenclature and classification for the astrophyllite-supergroup minerals. The HOH block is the main structural unit in all astrophyllite-supergroup structures; it consists of three H–O–H sheets where the T4O12 astrophyllite ribbons occur in the H sheets. In each structure, HOH blocks alternate with I (Intermediate) blocks along [001]. The twelve minerals of the astrophyllite supergroup are divided into three groups based on (1) the type of self-linkage of HOH blocks, i.e. (a) HOH blocks link directly where they share common vertices of D octahedra, or (b) HOH blocks do not link directly; and (2) the dominant cation of the O sheet (the C group: C7 apfu). In the astrophyllite group (HOH blocks connect via D– XPD–D bridges, Fe2+ is dominant at C7), there are six minerals: astrophyllite, niobophyllite, zircophyllite, tarbagataite, nalivkinite and bulgakite. In the kupletskite group (HOH blocks connect via D–XPD–D bridges, Mn2+ is dominant at C7), there are three minerals: kupletskite, niobokupletskite and kupletskite-(Cs). In the devitoite group (HOH blocks do not connect via D–XPD–D bridges), there are three minerals: devitoite, sveinbergeite and lobanovite. The general formula for the astrophyllite-supergroup minerals is of the form A2pBrC7D2(T4O12)2IXOD2XOA4XPDnWA2, where C [cations at the M(1–4) sites in the O sheet] = Fe2+, Mn, Na, Mg, Zn, Fe3+, Ca, Zr, Li; D (cations in the H sheets) = [6, 5]Ti, Nb, Zr, Sn4+, [5] Fe3+, Mg, Al; T = Si, minor Al; A2pBrIWA2Here we report a nomenclature and classification for the astrophyllite-supergroup minerals. The HOH block is the main structural unit in all astrophyllite-supergroup structures; it consists of three H–O–H sheets where the T4O12 astrophyllite ribbons occur in the H sheets. In each structure, HOH blocks alternate with I (Intermediate) blocks along [001]. The twelve minerals of the astrophyllite supergroup are divided into three groups based on (1) the type of self-linkage of HOH blocks, i.e. (a) HOH blocks link directly where they share common vertices of D octahedra, or (b) HOH blocks do not link directly; and (2) the dominant cation of the O sheet (the C group: C7 apfu). In the astrophyllite group (HOH blocks connect via D– XPD–D bridges, Fe2+ is dominant at C7), there are six minerals: astrophyllite, niobophyllite, zircophyllite, tarbagataite, nalivkinite and bulgakite. In the kupletskite group (HOH blocks connect via D–XPD–D bridges, Mn2+ is dominant at C7), there are three minerals: kupletskite, niobokupletskite and kupletskite-(Cs). In the devitoite group (HOH blocks do not connect via D–XPD–D bridges), there are three minerals: devitoite, sveinbergeite and lobanovite. The general formula for the astrophyllite-supergroup minerals is of the form A2pBrC7D2(T4O12)2IXOD2XOA4XPDnWA2, where C [cations at the M(1–4) sites in the O sheet] = Fe2+, Mn, Na, Mg, Zn, Fe3+, Ca, Zr, Li; D (cations in the H sheets) = [6, 5]Ti, Nb, Zr, Sn4+, [5] Fe3+, Mg, Al; T = Si, minor Al; A2pBrIWA2 (I block) where p = 1, 2; r = 1, 2; A = K, Cs, Ba, H2O, Li, Rb, Pb2+, Na, ; B = Na, Ca, Ba, H2O, ; I represents the composition of the central part of the I block, excluding peripheral layers of the form A2pBrWA2, e.g. (PO4)2(CO3) (devitoite); XOD = O; XOA = OH, F; XPD = F, O, OH, H2O, , where n = 0, 1, 2 for (XPD) n; WA = H2O, . … (more)
- Is Part Of:
- Mineralogical magazine. Volume 81:Number 1(2017)
- Journal:
- Mineralogical magazine
- Issue:
- Volume 81:Number 1(2017)
- Issue Display:
- Volume 81, Issue 1 (2017)
- Year:
- 2017
- Volume:
- 81
- Issue:
- 1
- Issue Sort Value:
- 2017-0081-0001-0000
- Page Start:
- 143
- Page End:
- 153
- Publication Date:
- 2017-02-01
- Subjects:
- Mineralogy -- Periodicals
Mineralogy -- Great Britain -- Periodicals
549.05 - Journal URLs:
- https://www.cambridge.org/core/journals/mineralogical-magazine ↗
http://pi2.ingenta.com/content/minsoc/mag;jsessionid=k179kevo8th.alice ↗ - DOI:
- 10.1180/minmag.2016.080.077 ↗
- Languages:
- English
- ISSNs:
- 0026-461X
- Deposit Type:
- Legaldeposit
- View Content:
- Available online (eLD content is only available in our Reading Rooms) ↗
- Physical Locations:
- British Library DSC - 5788.000000
British Library HMNTS - ELD Digital store - Ingest File:
- 8370.xml