Mid-ocean ridge and suprasubduction affinities in the ophiolitic belts of Albania

L. Beccaluva; M. Coltorti; I. Premti; E. Saccani; F. Siena; O. Zeda

Mid-ocean ridge and suprasubduction affinities in the ophiolitic belts of Albania

L. Beccaluva, M. Coltorti, I. Premti, E. Saccani, F. Siena, O. Zeda

Research output: Contribution to journal › Article › peer-review

Abstract

Petrological data based on 147 new major and trace element analyses are presented as a preliminary result of the research program on Jurassic ophiolites from Albania. Albanide ophiolites of the Mirdita tectonic zone represent one of the most complete, coherent sequences among all the Mediterranean ophiolites, and are constituted by two NNW-SSE trending subparallel belts, the Eastern Belt and the Western Belt. The petrological characteristics of the two belts are described, and a paleogeographic reconstruction of the Mirdita oceanic basin during the Jurassic is presented. -from Authors

Original language	English
Pages (from-to)	77-96
Number of pages	20
Journal	Ofioliti
Volume	19
Issue number	1
Publication status	Published - 1994
Externally published	Yes

Access to Document

Link to publication in Scopus

Fingerprint Dive into the research topics of 'Mid-ocean ridge and suprasubduction affinities in the ophiolitic belts of Albania'. Together they form a unique fingerprint.

Cite this

@article{7c227d54d205472b99b5c0e8945c9df7,

title = "Mid-ocean ridge and suprasubduction affinities in the ophiolitic belts of Albania",

abstract = "Petrological data based on 147 new major and trace element analyses are presented as a preliminary result of the research program on Jurassic ophiolites from Albania. Albanide ophiolites of the Mirdita tectonic zone represent one of the most complete, coherent sequences among all the Mediterranean ophiolites, and are constituted by two NNW-SSE trending subparallel belts, the Eastern Belt and the Western Belt. The petrological characteristics of the two belts are described, and a paleogeographic reconstruction of the Mirdita oceanic basin during the Jurassic is presented. -from Authors",

author = "L. Beccaluva and M. Coltorti and I. Premti and E. Saccani and F. Siena and O. Zeda",

year = "1994",

language = "English",

volume = "19",

pages = "77--96",

journal = "Ofioliti",

issn = "0391-2612",

publisher = "Pitagora Editrice",

number = "1",

}

TY - JOUR

T1 - Mid-ocean ridge and suprasubduction affinities in the ophiolitic belts of Albania

AU - Beccaluva, L.

AU - Coltorti, M.

AU - Premti, I.

AU - Saccani, E.

AU - Siena, F.

AU - Zeda, O.

PY - 1994

Y1 - 1994

N2 - Petrological data based on 147 new major and trace element analyses are presented as a preliminary result of the research program on Jurassic ophiolites from Albania. Albanide ophiolites of the Mirdita tectonic zone represent one of the most complete, coherent sequences among all the Mediterranean ophiolites, and are constituted by two NNW-SSE trending subparallel belts, the Eastern Belt and the Western Belt. The petrological characteristics of the two belts are described, and a paleogeographic reconstruction of the Mirdita oceanic basin during the Jurassic is presented. -from Authors

AB - Petrological data based on 147 new major and trace element analyses are presented as a preliminary result of the research program on Jurassic ophiolites from Albania. Albanide ophiolites of the Mirdita tectonic zone represent one of the most complete, coherent sequences among all the Mediterranean ophiolites, and are constituted by two NNW-SSE trending subparallel belts, the Eastern Belt and the Western Belt. The petrological characteristics of the two belts are described, and a paleogeographic reconstruction of the Mirdita oceanic basin during the Jurassic is presented. -from Authors

UR - http://www.scopus.com/inward/record.url?scp=0028594643&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0028594643

VL - 19

SP - 77

EP - 96

JO - Ofioliti

JF - Ofioliti

SN - 0391-2612

IS - 1

ER -