First International Conference on MOLDAVIAN RISKS – FROM ...
First International Conference on MOLDAVIAN RISKS – FROM ... First International Conference on MOLDAVIAN RISKS – FROM ...
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<str<strong>on</strong>g>First</str<strong>on</strong>g> <str<strong>on</strong>g>Internati<strong>on</strong>al</str<strong>on</strong>g> <str<strong>on</strong>g>C<strong>on</strong>ference</str<strong>on</strong>g> <strong>on</strong> <strong>MOLDAVIAN</strong> <strong>RISKS</strong> - <strong>FROM</strong> GLOBAL TO LOCAL SCALE<br />
16-19 May 2012, Bacau, Romania<br />
PLIO-PLEISTOCENE CONNECTION BETWEEN THE<br />
‘VRANCEA ZONE’ AND THE SOUTHERN END OF THE<br />
HARGHITA VOLCANIC CHAIN<br />
Seghedi Ioan 1 1, 2<br />
, Szakács Alexandru<br />
1 Institute of Geodynamics, Romanian Academy, Bucharest, Romania<br />
2 Sapientia University, Dept. of Envir<strong>on</strong>mental Sciences, Cluj-Napoca, Romania<br />
Seghedi Ioan, seghedi@geodin.ro<br />
Abstract: Miocene c<strong>on</strong>vergence at ~ 11 Ma of the Eastern Carpathian orogen of Romania<br />
caused the tect<strong>on</strong>ic nappes emplacement of the fold - thrust belt. The following postcollis<strong>on</strong>al<br />
complex tect<strong>on</strong>ic crustal deformati<strong>on</strong> in this area resulted in Late Miocene to<br />
Quaternary formati<strong>on</strong> of the Cǎlimani-Gurghiu-Harghita volcanic chain. This was possibly<br />
related to clockwise rotati<strong>on</strong> and fr<strong>on</strong>t block-fragmentati<strong>on</strong> of the inner Carpathian (Dacia)<br />
crustal block. The Carpathian foreland is characterized by a mechanically str<strong>on</strong>g and cold<br />
European-Scythian Plate welded to the south with weak Moesian plate al<strong>on</strong>g the Trotuş<br />
transverse high angle basement fault system that was reactivated and decoupled from it<br />
during Late Pliocene-Quaternary. This period was characterized by differential vertical<br />
movements of the Moesian plate associated with ~5km of c<strong>on</strong>tracti<strong>on</strong> restricted roughly<br />
between the Trotuş and Intramoesian faults and sustained by the apparently folded, shallow<br />
Moho beneath the orogen and the generati<strong>on</strong> of ‘Vrancea z<strong>on</strong>e’. In the same period after a<br />
time gap Plio-Quaternary magmatic activity in the interior of the Carpathians area, in close<br />
proximity to the ‘Vrancea z<strong>on</strong>e’, shows a shift from normal calc-alkaline to a diverse<br />
compositi<strong>on</strong>s (adakite-like calc-alkaline, K-alkalic, in South Harghita Mountains and mafic<br />
Na-alkalic in Perşani Mountains). This magmatism is interpreted to be in close c<strong>on</strong>necti<strong>on</strong><br />
to steepening of ‘Vrancea z<strong>on</strong>e’ via tearing or delaminati<strong>on</strong> of its eclogitic keel and partial<br />
melting of this material at mantle depths to explain the peculiar chemistry of adakite-like<br />
volcanic rocks as a c<strong>on</strong>sequence of elevated K2O/Na2O in the protolith and high pressure<br />
c<strong>on</strong>diti<strong>on</strong>s of partial melting. The surface projecti<strong>on</strong> of the South Harghita adakite-like<br />
calc-alkaline volcanism at the edge of ‘Vrancea z<strong>on</strong>e’, as a piece of metasomatised<br />
lithosphere can be explained by its heating and partial melting during the horiz<strong>on</strong>tal<br />
asthenospheric flow around the steepening z<strong>on</strong>e. The Na-alkalic mafic magmas were<br />
derived from such an uprised asthenospheric mantle-source by decompressi<strong>on</strong> melting that<br />
correlates with a low-velocity anomaly and with a high attenuati<strong>on</strong> volume, as indicated by<br />
the geophysical observati<strong>on</strong>s. Generati<strong>on</strong> of K and Na alkalic magmas in the similar time<br />
interval, by interrupting the adakite-like volcanism signifies changes in the source and<br />
melting mechanism by renewed c<strong>on</strong>tracti<strong>on</strong> associated with deep mantle processes<br />
facilitated by the generalized tect<strong>on</strong>ic inversi<strong>on</strong> event which started during the latest<br />
Pliocene in the whole Carpathian<strong>–</strong>Pann<strong>on</strong>ian regi<strong>on</strong>.<br />
Key words: Post-collisi<strong>on</strong>al magmatism, slab mechanics, calc-alkaline adakite magmas, K and Na<br />
alkalic magmas.<br />
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