01.09.2013 Views

DACIAN BASIN - GeoEcoMar

DACIAN BASIN - GeoEcoMar

DACIAN BASIN - GeoEcoMar

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

References<br />

Ji P A d. C., ol A r i u C., mAr inesCu n., ol t e A n u r., Br u s t u r t., 2007. A Late Neogene marker sequence in<br />

the Dacian Basin (Paratethys realm). Genetic and stratigraphic significance. Geo-Eco-Marina,<br />

13:121-138. Bucharest<br />

Ju h á s Z, g., Po g á C s á s, g., mA g y A r, i., VA K A r C s g., 2007. Tectonic versus climatic control on the evolution<br />

of fluvio-deltaic systems in a lake basin, Eastern Pannonian Basin. Sedimentary Geology, 202:<br />

72–95.<br />

Ko n e r d i n g, C., di n u, C., wo n g, h. K., in press. Seismic stratigraphy, structure and Mio-Pleistocene subsidence<br />

of the romanian Black Sea shelf. in Sedimentary Basin Tectonics from the Black Sea<br />

and Caucasus to the Arabian Platform, r. A. Stephenson, V. i. Starostenko (eds.). Special publication,<br />

Geological Society of London<br />

Kr iJ g s m A n , w., 1996. Miocene magnetostratigraphy and cyclostratigraphy in the Mediterranean: Extension<br />

of the Astronomical Polarity Time Scale, PhD Thesis, Geologica Ultraiectina, 141. 207 pp<br />

lA s K A r e V V., 1924. Sur les equivalents du Sarmatien superieur en Serbie. recueil de traveaux offerts a<br />

Jovan Civisic: 73-85. Drzhavna Shtamparija. Beograd<br />

leeVer, K.A., mA t e n C o, l., Be r to t t i, g., Cl o e t i n g h, s., dr iJ K o n i n g e n, g. g., 2006. Late orogenic vertical movements<br />

in the Carpathian Bend Zone - seismic constraints on the transition zone from orogen to<br />

foredeep, Basin research, 18: 521-545<br />

leVeer, K. A., 2007. Foreland of the romanian Carpathians. Controls on late orogenic sedimentary<br />

basin evolution and Paratethys paleogeography. Thesis. Vrije Universiteit 182. Amsterdam<br />

li t eA n u, e., roşCulesCu, e., Fe r u, m., AndreesCu, i., 1968. Succesiunile litologice şi fauna de moluşte care<br />

caracterizează limita Pliocen-Pleistocen din zona Pleşcoi (V. Buzăului). Studii şi Cercetări de Geologie,<br />

Geofizică şi Geografie, Ser. Geol., 13, 2: 539-545<br />

lo u r e n s, l.J., hi l g e n, F.J., ZA C h A r iA s s e, w.J., V A n hoo F, A.A.m., An t o n A r A K o u, A., Ve r g n A u d-gr A Z Z i n i, C.,1996<br />

– Evaluation of the Pliocene to early Pleistocene astronomical time scale, Paleoceanography,<br />

11: 391-413<br />

lo u r e n s, l.J., hi l g e n, F.J., lA s K A r, J., sh A C K l e t o n, n.J., wi l s o n, d., 2004. The Neogene period. in Gradstein, F.M.,<br />

Ogg, J.G., Smith, A.G. (eds.), A Geologic Time Scale 2004, Cambridge University Press: 409-440<br />

luBenesCu, V., 2004. Limita Dacian/romanian. in Pliocenul superior din Bazinul Dacic (Etajul romanian).<br />

Faună, Stratirafie, Sedimentogeneză: 41-47. Acad. romana, Emil racovita inst.of Speology.<br />

Bucuresti<br />

mA t e n C o, l., Be r to t t i, g., leeVer, K., Cl o e t i n g h, s., sC h m i d, s., tă r ă P o A n C ă, m., di n u, C., 2007. Large-scale deformation<br />

in a locked collisional boundary: interplay between subsidence and uplift, intraplate<br />

stress, and inherited lithospheric structure in the late stage of the SE Carpathians evolution,<br />

Tectonics, 26, 4:1-29<br />

mA C A r o V iC i, n., 1961. Observaţii stratigrafice pe structura Berca-Arbănaşi cu privire specială asupra<br />

limitelor Dacianului. St. Cerc Geol. Vi, 3. Bucureşti<br />

mA C A r o V iC i, n., mAr inesCu, F., mo t A ş, i., 1965. Aperçu sur le Néogène superieur et le Pontien s. str. du<br />

Bassin Dacique. rev. roum. Géol., Géophys., Géogr., Série Géol., 10, 2: 185-195. Bucharest<br />

259

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!