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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F11%3A00000417%21RIV12-MZP-00025798
rdf:type
skos:Concept n10:Vysledek
dcterms:description
We examined the tectono-metamorphic evolution of the contact aureole around the Cretaceous Dipilto Batholith in the Eastern Chortis Terrane. Three distinct metamorphic phases were distinguished. The first phase represented greenschist-facies regional metamorphism (M1) accompanied by a prograde deformation (D1). The Cretaceous contact-metamorphic event (M2) produced the peak-metamorphic mineral assemblages Wo + Di + Grs + Ves + Qtz + Pl + Kfs in the calc-silicate rocks and Bt + Qtz + Ab + And ± Crd ± Gr ± Chl ± Ms ± Kfs in the metapelites. The estimated P–T conditions near the contact with granitoids are 500–650 °C and ~ 0.2 GPa and coexisting fluids were relatively poor in CO2. The emplacement of the Dipilto Batholith at shallow crustal levels was rarely accompanied by weak deformation of the metasediments (D2). During cooling and exhumation, the contact aureole was locally affected by deformation (D3) and retrograde metamorphism (M3) again under greenschist-facies conditions. We examined the tectono-metamorphic evolution of the contact aureole around the Cretaceous Dipilto Batholith in the Eastern Chortis Terrane. Three distinct metamorphic phases were distinguished. The first phase represented greenschist-facies regional metamorphism (M1) accompanied by a prograde deformation (D1). The Cretaceous contact-metamorphic event (M2) produced the peak-metamorphic mineral assemblages Wo + Di + Grs + Ves + Qtz + Pl + Kfs in the calc-silicate rocks and Bt + Qtz + Ab + And ± Crd ± Gr ± Chl ± Ms ± Kfs in the metapelites. The estimated P–T conditions near the contact with granitoids are 500–650 °C and ~ 0.2 GPa and coexisting fluids were relatively poor in CO2. The emplacement of the Dipilto Batholith at shallow crustal levels was rarely accompanied by weak deformation of the metasediments (D2). During cooling and exhumation, the contact aureole was locally affected by deformation (D3) and retrograde metamorphism (M3) again under greenschist-facies conditions.
dcterms:title
Metamorphic evolution of the contact aureole of the Dipilto Batholith, Eastern Chortis Terrane, Nicaragua Metamorphic evolution of the contact aureole of the Dipilto Batholith, Eastern Chortis Terrane, Nicaragua
skos:prefLabel
Metamorphic evolution of the contact aureole of the Dipilto Batholith, Eastern Chortis Terrane, Nicaragua Metamorphic evolution of the contact aureole of the Dipilto Batholith, Eastern Chortis Terrane, Nicaragua
skos:notation
RIV/00025798:_____/11:00000417!RIV12-MZP-00025798
n10:predkladatel
n11:ico%3A00025798
n3:aktivita
n9:S n9:P n9:V
n3:aktivity
P(GP205/07/P130), S, V
n3:cisloPeriodika
2011
n3:dodaniDat
n17:2012
n3:domaciTvurceVysledku
n19:6772676
n3:druhVysledku
n8:J
n3:duvernostUdaju
n16:S
n3:entitaPredkladatele
n15:predkladatel
n3:idSjednocenehoVysledku
211731
n3:idVysledku
RIV/00025798:_____/11:00000417
n3:jazykVysledku
n6:eng
n3:klicovaSlova
low-pressure metamorphism, fluid inclusions, calc-silicate rocks, Dipilto Batholith, Nicaragua, Eastern Chortis Terrane
n3:klicoveSlovo
n4:Dipilto%20Batholith n4:Nicaragua n4:Eastern%20Chortis%20Terrane n4:fluid%20inclusions n4:low-pressure%20metamorphism n4:calc-silicate%20rocks
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[5207CF119B43]
n3:nazevZdroje
Journal of Geosciences
n3:obor
n13:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
2
n3:projekt
n14:GP205%2F07%2FP130
n3:rokUplatneniVysledku
n17:2011
n3:svazekPeriodika
56
n3:tvurceVysledku
Dolníček, Zdeněk Buriánek, David
n3:wos
000290046200002
s:issn
1802-6222
s:numberOfPages
17
n18:doi
10.3190/jgeosci.084