The timing of the tectono-metamorphic evolution at the Neoproterozoic-Phanerozoic boundary in central southern Madagascar

TY - JOUR

T1 - The timing of the tectono-metamorphic evolution at the Neoproterozoic-Phanerozoic boundary in central southern Madagascar

AU - Giese, Jörg

AU - Berger, Alfons

AU - Schreurs, Guido

AU - Gnos, Edwin

PY - 2011/3/11

Y1 - 2011/3/11

N2 - In central southern Madagascar the crystalline basement is composed of mid-crustal rocks which have experienced polycyclic deformation and metamorphism coupled with repeated granitoid magmatism at the Neoproterozoic–Phanerozoic boundary. Based on the integration of in situ U–Th–Pb dating of monazite and structural relationships,twodistinct phases of major ductile deformation, the Andreaba and Ihosy phases can be distinguished in central southern Madagascar. Both these deformation phases occur between ~550 and 520 Ma. Coeval with, and outlasting deformation, granitic plutons and dykes were emplaced. HT/HP granulite facies metamorphism (M1), including migmatisation and anatexis of the crust started at~585Maand lasted until at least~500 Ma. Monazite growth between 480 and 450Mapostdates major ductile deformation and might be related to a second, HT/MP metamorphism (M2), indicating that the whole crustal section remained in a mid-crustal position. Metamorphic overprinting related to M2 is spatially limited and is heterogeneously distributed in central southern Madagascar. Newly developed M2 mineral assemblages are preferentially found in areas featuring Ihosy phase vertical foliation planes. Very often these structures show brittle/ductile or brittle overprint and might be considered as preferred pathways for fluid flow, thus localising metamorphic overprint.

AB - In central southern Madagascar the crystalline basement is composed of mid-crustal rocks which have experienced polycyclic deformation and metamorphism coupled with repeated granitoid magmatism at the Neoproterozoic–Phanerozoic boundary. Based on the integration of in situ U–Th–Pb dating of monazite and structural relationships,twodistinct phases of major ductile deformation, the Andreaba and Ihosy phases can be distinguished in central southern Madagascar. Both these deformation phases occur between ~550 and 520 Ma. Coeval with, and outlasting deformation, granitic plutons and dykes were emplaced. HT/HP granulite facies metamorphism (M1), including migmatisation and anatexis of the crust started at~585Maand lasted until at least~500 Ma. Monazite growth between 480 and 450Mapostdates major ductile deformation and might be related to a second, HT/MP metamorphism (M2), indicating that the whole crustal section remained in a mid-crustal position. Metamorphic overprinting related to M2 is spatially limited and is heterogeneously distributed in central southern Madagascar. Newly developed M2 mineral assemblages are preferentially found in areas featuring Ihosy phase vertical foliation planes. Very often these structures show brittle/ductile or brittle overprint and might be considered as preferred pathways for fluid flow, thus localising metamorphic overprint.

U2 - 10.1016/j.precamres.2011.01.002

DO - 10.1016/j.precamres.2011.01.002

M3 - Journal article

SN - 0301-9268

VL - 185

SP - 131

EP - 148

JO - Precambrian Research

JF - Precambrian Research

IS - 3-4

ER -