Nalazite se na CroRIS probnoj okolini. Ovdje evidentirani podaci neće biti pohranjeni u Informacijskom sustavu znanosti RH. Ako je ovo greška, CroRIS produkcijskoj okolini moguće je pristupi putem poveznice www.croris.hr
izvor podataka: crosbi !

Krk impact structure ejecta breccia and melt rocks on the island of Rab, Croatian Adriatic: a clue on the impact target lithology (CROSBI ID 635735)

Prilog sa skupa u zborniku | sažetak izlaganja sa skupa

Marjanac, Tihomir ; Tomša, Ana Marija ; Marjanac, Ljerka ; Čalogović, Marina ; Fazinić, Stjepko Krk impact structure ejecta breccia and melt rocks on the island of Rab, Croatian Adriatic: a clue on the impact target lithology // Bridging The Gap III: Impact cratering in nature, experiment and modelling. Freiburg, 2015. str. 1-1

Podaci o odgovornosti

Marjanac, Tihomir ; Tomša, Ana Marija ; Marjanac, Ljerka ; Čalogović, Marina ; Fazinić, Stjepko

engleski

Krk impact structure ejecta breccia and melt rocks on the island of Rab, Croatian Adriatic: a clue on the impact target lithology

The study of the proposed Krk impact structure ejecta was conducted on the surrounding northern Adriatic islands of Cres, St. Grgur, Goli and Rab, as well as along the mainland coast. At all of these localities, limestone breccia veneer was found disconformably overlying geological structures, and attributed to the informal unit of Krk-breccia (though on the Rab island it is usually referred to as Rab-breccia). Unlike Jelar-breccia which occurs along the Velebit Mt. front, the Krk-breccia comprises boulder-size clasts of Eocene sandstones and marls with the Krk island provenance. The impact melts are found on eastern coasts of the Krk and Rab islands, but only in secondary position. At one Rab island locality, contact thermal metamorphosis of sandstone base-rock was found, indicating its progressive melting from the surface downwards. Two types of melts can be differentiated ; i) incomplete melts with remnants of unmelted sandstones, usually with melted rims, and ii) massive crystalline glass, sometimes with flow structures. The massive glass is found on the Rab island and occurs in form of small boulder chunks, 10-30 kg in weight. These were found to lay above Eocene siliceous sandstones, and some glass blocks were embedded in an old Roman wall. The glass is dark bluish in colour, crystalline with olivines predominating, massive and only locally vesicular. The chemical composition of glass shows predominance of iron (73 % in average), whereas vesicles are sometimes filled with secondary carbonate.

Krk island ; impact structure ; impact breccia ; melt-rocks ; impact glesses ; provenance

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o prilogu

1-1.

2015.

objavljeno

Podaci o matičnoj publikaciji

Bridging The Gap III: Impact cratering in nature, experiment and modelling

Freiburg:

Podaci o skupu

Bridging The Gap III: Impact cratering in nature, experiment and modelling.

poster

21.09.2015-26.09.2015

Freiburg, Njemačka

Povezanost rada

Geologija