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⇱ Grossular from Cimino Volcanic Complex, Viterbo Province, Lazio, Italy

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Grossular from
Cimino Volcanic Complex, Viterbo Province, Lazio, Italy

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Locality type:Complex
Classification
Species:Grossular
Formula:Ca3Al2(SiO4)3
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Grossular data
Locality Data:Click here to view Cimino Volcanic Complex, Viterbo Province, Lazio, Italy
Data Identifiers
Mindat Occurrence Record ID:1308808
Long-form Identifier:1:3:1308808:0
GUID (UUID V4):0
References
Reference Search (possible matching items)
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Journal (issue)
collection. Photo: Michael B. Leybov. Title PagePhoto Complex calcite tvlin on marcasite.Specimen 6 x 7 x 3 cm...Minerals from the Sacrofano Caldera, Rome, Latium, Italy ....................... 20 The Great Break in...Kaltsytovyi nugget is a precious print from the vein of complex shape. Its walls were covered by quartz and calcite...MINERALS FROMTHE SACROFANO CALDERA, ROME,LATIUM,ITALY Nikita V. Chukanov,RobertoAllori 12 Perugia 0...collectors for a long time. It is a classical young volcanic area and type locality of seven new mineral species
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Journal (article/letter/editorial)
Although usually classed as orogenic lavas, these volcanic SC RI rocks may result from re-melting of newly...fluxes are compositionally well matched with arc volcanic outputs in terms of trace elements such as La...temperature and pressure, especially in pyrope and grossular content (Auzanneau et al., 2006). Pyrope content...whereas almandine content fluctuates. At 2 GPa, grossular drops appreciably as temperature climbs, probably...51% 48% 60% 55% 0% 0% 2% 0% 0% 0% 2% Grossular 6% 6% 4% 20% 17% 7% 13% Pyrope 40% 33%
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Journal (issue)
Scienze della Terra, Univ. of Milan, 20133 Milano Italy: PROF. ICHIRO SUNAGAWA, Kashiwa-cho 3-54-2, Tachikawa...the Blekinge province is not a southerly continuation o f the Svccokarclian orogenic province o f central...t can be correlated with the SW Swedish gneiss province, formed 1800-1650 m.y. ago. Rb-Sr whole-rock isochron...the mafic and ultramafic magmas o f the lower volcanic sequence of the Kuhmo—Suomussalmi greenstonc belt...favours a basement source which was part of an arc complex to the north rather than from the Dalradian block
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