. "[5207CF119B43]" . "low-pressure metamorphism, fluid inclusions, calc-silicate rocks, Dipilto Batholith, Nicaragua, Eastern Chortis Terrane"@en . "Doln\u00ED\u010Dek, Zden\u011Bk" . . "2"^^ . . "Metamorphic evolution of the contact aureole of the Dipilto Batholith, Eastern Chortis Terrane, Nicaragua"@en . "1"^^ . "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 \u00B1 Crd \u00B1 Gr \u00B1 Chl \u00B1 Ms \u00B1 Kfs in the metapelites. The estimated P\u2013T conditions near the contact with granitoids are 500\u2013650 \u00B0C 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."@en . "2011" . . "RIV/00025798:_____/11:00000417" . "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 \u00B1 Crd \u00B1 Gr \u00B1 Chl \u00B1 Ms \u00B1 Kfs in the metapelites. The estimated P\u2013T conditions near the contact with granitoids are 500\u2013650 \u00B0C 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." . . . . "Buri\u00E1nek, David" . . "56" . . . "17"^^ . . "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" . "211731" . "RIV/00025798:_____/11:00000417!RIV12-MZP-00025798" . . . "Metamorphic evolution of the contact aureole of the Dipilto Batholith, Eastern Chortis Terrane, Nicaragua"@en . . "CZ - \u010Cesk\u00E1 republika" . . "Journal of Geosciences" . . . "10.3190/jgeosci.084" . "000290046200002" . "1802-6222" . . "P(GP205/07/P130), S, V" .