dc.contributor.author | Fonteilles, M | |
dc.contributor.author | Forette, MC | |
dc.contributor.author | Berson, F | |
dc.contributor.author | Pascal, ML | |
dc.contributor.author | Ongen, S | |
dc.contributor.author | Demange, M | |
dc.date.accessioned | 2021-03-04T11:51:29Z | |
dc.date.available | 2021-03-04T11:51:29Z | |
dc.date.issued | 1998 | |
dc.identifier.citation | Demange M., Berson F., Fonteilles M., Pascal M., Ongen S., Forette M., "Wollastonite-garnet skarns of Demir Tepe, Tahtakopru (province of Bursa, Turkey)", COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES, cilt.326, sa.11, ss.771-778, 1998 | |
dc.identifier.issn | 1251-8050 | |
dc.identifier.other | av_7474bd58-8895-44c5-8462-b1ff9d2a0e38 | |
dc.identifier.other | vv_1032021 | |
dc.identifier.uri | http://hdl.handle.net/20.500.12627/80045 | |
dc.identifier.uri | https://doi.org/10.1016/s1251-8050(98)80242-5 | |
dc.description.abstract | Wollastonite-garnet skarns of Demir Tepe (Turkey) are developed in graphitic marbles, forming roof-pendants in the granodioritic Tertiary pluton of Goynukbelen, at the contact of stocks and veins of diorite-monzodiorites that intrude the main pluton. Skarn formation includes several superposed stages | |
dc.language.iso | eng | |
dc.subject | Temel Bilimler (SCI) | |
dc.subject | Jeoloji Mühendisliği | |
dc.subject | YER BİLİMİ, MULTİDİSİPLİNER | |
dc.subject | Yerbilimleri | |
dc.subject | JEOLOJİ | |
dc.subject | Mühendislik ve Teknoloji | |
dc.title | Wollastonite-garnet skarns of Demir Tepe, Tahtakopru (province of Bursa, Turkey) | |
dc.type | Makale | |
dc.relation.journal | COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES | |
dc.contributor.department | , , | |
dc.identifier.volume | 326 | |
dc.identifier.issue | 11 | |
dc.identifier.startpage | 771 | |
dc.identifier.endpage | 778 | |
dc.contributor.firstauthorID | 120892 | |