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Amphibole Supergroup from
Basaltic lava flow, Valle Gran Rey, La Gomera, Santa Cruz de Tenerife Province, Canary Islands, Spain


Locality type:Lava Flow
Classification
Species:'Amphibole Supergroup' (not an IMA approved species)
Formula:AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Amphibole Supergroup data
Locality Data:Click here to view Basaltic lava flow, Valle Gran Rey, La Gomera, Santa Cruz de Tenerife Province, Canary Islands, Spain
Data Identifiers
Mindat Occurrence Record ID:311217
Long-form Identifier:1:3:311217:5
GUID (UUID V4):a8d22f62-9eb1-48e7-b79e-5fbcf98d5d45
Nearest other occurrences of Amphibole Supergroup
14.0km (8.7 miles) ⓘVallehermoso beach dykes, Vallehermoso, La Gomera, Santa Cruz de Tenerife Province, Canary Islands, Spain
77.9km (48.4 miles) ⓘTajogaite Volcano, Cumbre Vieja Area, La Palma, Santa Cruz de Tenerife Province, Canary Islands, Spain
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
complex, such as the Kuh-e Qarineh cone in where basaltic scoriaceous falls are underlain by felsic pyroclastic...eruption columns and are overlain by basaltic lava flows linked to basaltic fire fountains. Thus, it seems...with the same paragenesis as the basaltic scoriaceous falls and lava flows. Three classes of cumulates...biotitite. Moreover, the mineral assemblage of basaltic rocks in the area (olivine ­(Fo79 − 83) + diopside...trend, the whole-rock and mineral chemistry of the basaltic Editorial handling: L. Danyushevsky * Abbas Asiabanha
Journal (article/letter/editorial)
and figures are: Ab—albite, Act—actinolite, Amp—amphibole, Ap—apatite, Cal—calcite, Cel—celadonite, Chl—chlorite...and some schistose limestones with basalts and basaltic tuff layers of the DĂșbrava or Hačava formations...reported from the overlying Torna/Turňa Nappe [87]. Amphibole gabbros to dolerites and serpentinites are embedded...sediments at DobĆĄinĂĄ [8]. The 135 Ma U–Pb SIMS [92] and LA–ICP–MS [73] age of metamorphic–metasomatic Prv (ΔNd135...shales, and pale-red radiolarites radiolarites with basaltic tuff layers (Figure 7d). Regularly alternating
 
Mineral and/or Locality  
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