1977
DOI: 10.1007/bf01081744
|View full text |Cite
|
Sign up to set email alerts
|

Petrochemistry of low and medium grade mafic metamorphic rocks from Leros island, Greece

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
2
1

Citation Types

0
5
0

Year Published

1980
1980
2021
2021

Publication Types

Select...
6

Relationship

0
6

Authors

Journals

citations
Cited by 6 publications
(5 citation statements)
references
References 13 publications
0
5
0
Order By: Relevance
“…Katagas (1984) described the Eocene high-P/T metamorphism that formed PA, BS, and GS mineral parageneses on the island of Jaros. Similar metamorphic aspects are observed in Leros Island, where A-type protoliths are converted into schists under BS/GS-transition to EA-facies conditions (Katagas and Sapountzis, 1977).…”
Section: Iberian Peninsulamentioning
confidence: 65%
“…Katagas (1984) described the Eocene high-P/T metamorphism that formed PA, BS, and GS mineral parageneses on the island of Jaros. Similar metamorphic aspects are observed in Leros Island, where A-type protoliths are converted into schists under BS/GS-transition to EA-facies conditions (Katagas and Sapountzis, 1977).…”
Section: Iberian Peninsulamentioning
confidence: 65%
“…It consists of interlayered phyllites, micaschists, quarzites and marbles with rare occurrences of metabasites. The presence of Mg-riebeckite, glaucophane and aragonite in Leros and Arki islands [Katagas & Sapountzis, 1977;Katagas, 1980;Franz & Okrusch, 1992;Roche et al, 2018a], implies a subduction-related metamorphism with a A C C E P T E D M A N U S C R I P T 12 minimum pressure of ~ 8 kbar. Roche et al [2018a] show that glaucophane/Mg-riebeckite is locally preserved and may destabilize into winchite, suggesting a greenschist-facies overprint.…”
Section: Dodecanese Islandsmentioning
confidence: 99%
“…Very few studies were published on the geology of Leros Island. Katagas and Sapountzis (1977) distinguished four tectono-metamorphic units, which Franz et al (2005) then grouped in only two, Temenia and Marina units, covered with a sedimentary unit attributed to the Miocene. Marina unit, further divided into two subunits, Panormos and Emporios (Franz et al 2005), is composed of amphibolites and garnet-micaschists (pre-…”
Section: The Dodecanese Archipelagomentioning
confidence: 99%