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Magmatic activity migrated from North to South and built the following volcanic centres: Jirca (J), Fancel-Lapusna (FL), Bacta (B), Seaca-Tatarea (ST), Borzont (BZ), Sumuleu (S) and Ciumani-Fierastraie (CF). The timing of volcanic activity in each volcanic centre reflects the previously recognized overlapping age progression from North to South along the arc: J = 9.2-7.0 Ma; FL = 9.4-6.0 Ma; B = 7.5-7.0 Ma; ST = 7.3-5.4 Ma; BZ = 6.8 Ma; S = 6.8-6.2 Ma; CF = 7.1-6.3 Ma. Two peripheral small intrusive bodies have also been dated (Ditrau - 7.9 Ma and Corund - 7.4 Ma). The duration of volcanic activity of each centre is ca. 1 Ma, with a larger interval of 2.5 Ma for the Fancel-Lapusna volcano. Volcanic activity in the southernmost volcanic centres (ST; BZ; S; CF) between 7-6 Ma was contemporaneous. Certain volcanological problems are pointed out: (i) the voluminous debris-avalanche deposit assumed to belong to the Calimani Mountains includes blocks of ca. 8 Ma up to the Gurghiu Valley and between 7.5-7.8 Ma south of the Gurghiu Valley (ii) the Fancel-Lapusna caldera was generated around 6.9 Ma and involved a post-caldera uplift and/or erosion of the caldera floor and younger domes; and (iii) the model based on volcanic facies distribution is consistent with the new age-data.", "subjects" : [ { "otype" : "Classification", "mtid" : 10399, "link" : "/api/classification/10399", "label" : "Föld- és kapcsolódó környezettudományok", "published" : true, "snippet" : true } ], "digital" : null, "printed" : null, "sourceYear" : 2010, "packet" : "TPA_ATKI_alltype_2004.txt", "foreignEdition" : true, "foreignLanguage" : true, "fullPublication" : true, "conferencePublication" : false, "nationalOrigin" : true, "missingAuthor" : false, "oaType" : "GOLD", "oaCheckDate" : "2024-03-26", "oaFree" : 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