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Clinopyroxene Subgroup from
Bucak Lava Field, Bucak District, Burdur Province, Turkey


Locality type:Lava Field
Classification
Species:'Clinopyroxene Subgroup' (not an IMA approved species)
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Clinopyroxene Subgroup data
Locality Data:Click here to view Bucak Lava Field, Bucak District, Burdur Province, Turkey
Data Identifiers
Mindat Occurrence Record ID:1357443
Long-form Identifier:1:3:1357443:5
GUID (UUID V4):0
Nearest other occurrences of Clinopyroxene Subgroup
8.7km (5.4 miles) ⓘAksu Diamas project, Isparta Province, Turkey
30.4km (18.9 miles) ⓘGölcük Maar Crater, Gölcük District, Isparta Province, Turkey
83.6km (52.0 miles) ⓘCovur Yokusutepe Hill, Doganbaba, Yeşilova District, Burdur Province, Turkey
References
Lefevre, C., Bellon, H., & Poisson, A. (1983). Presence de leucitites dans le volcanisme Pliocene de la region d'Isparta (Taurides Occidentales, Turquie). Comptes-rendus des séances de l'Académie des sciences. Série 2, Mécanique-physique, chimie, sciences de l'univers, sciences de la terre, 297(4), 367-372.
Çoban, H., & Flower, M. F. (2006). Mineral phase compositions in silica-undersaturated ‘leucite’lamproites from the Bucak area, Isparta, SW Turkey. Lithos, 89(3-4), 275-299.
Çoban, H., & Flower, M. F. (2007). Late Pliocene lamproites from Bucak, Isparta (southwestern Turkey): implications for mantle ‘wedge’evolution during Africa-Anatolian plate convergence. Journal of Asian Earth Sciences, 29(1), 160-176.
Prelević, D., Akal, C., Foley, S. F., Romer, R. L., Stracke, A., Van Den Bogaard, P. (2012) Ultrapotassic Mafic Rocks as Geochemical Proxies for Post-collisional Dynamics of Orogenic Lithospheric Mantle: the Case of Southwestern Anatolia, Turkey. Journal of Petrology, 53 (5) 1019-1055 doi:10.1093/petrology/egs008
Fritschle, Tobias, Prelević, Dejan, Foley, Stephen F., Jacob, Dorrit E. (2013) Petrological characterization of the mantle source of Mediterranean lamproites: Indications from major and trace elements of phlogopite. Chemical Geology, 353. 267-279 doi:10.1016/j.chemgeo.2012.09.006
 
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