Evolución de paleoesfuerzos durante la exhumación de mármoles de alta presión, Complejo de Samaná, norte de La Española

  1. F.J. Fernández 1
  2. I. Rodriguez 6
  3. J. Escuder-Viruete 2
  4. A. Pérez-Estaún 3
  5. E. Mariani 4
  6. D. Prior 5
  1. 1 Universidad de Oviedo
    info

    Universidad de Oviedo

    Oviedo, España

    ROR https://ror.org/006gksa02

  2. 2 Instituto Geológico y Minero de España
    info

    Instituto Geológico y Minero de España

    Madrid, España

    ROR https://ror.org/04cadha73

  3. 3 ) Instituto de Ciencias de la Tierra “Jaume Almera” CSIC
  4. 4 Department of Earth, Ocean and Ecological Sciences
  5. 5 Geology Department, University of Otago
  6. 6 Universidad de León
    info

    Universidad de León

    León, España

    ROR https://ror.org/02tzt0b78

Aldizkaria:
Boletín geológico y minero

ISSN: 0366-0176

Argitalpen urtea: 2017

Alea: 128

Zenbakia: 3

Orrialdeak: 587-610

Mota: Artikulua

DOI: 10.21701/BOLGEOMIN.128.3.004 DIALNET GOOGLE SCHOLAR lock_openSarbide irekia editor

Beste argitalpen batzuk: Boletín geológico y minero

Laburpena

The marble of the Samaná complex presents a widespread foliation formed during its exhumation following a general decompressive strain path from high pressure (2.0P0.7 GPa) and low temperature (500 ºC) conditions. The foliation is plano-linear and blastomylonitic. Deformation distribution is highly heterogeneous. Calcite preferred orientation is poor, even though the marble has a well-defined tectonic fabric. The blastomylonitic fabric is masking an earlier tectonic fabric. Cathodoluminiscence images reveal that intense fracturing formed prior to foliation development in the marbles. The thermodynamic modelling of mineral phase transformations during prograde metamorphism indicate an increase in water content (1.2w.t. H2O1.8) that may have involved an increase in fluid pressure and triggered rock embrittlement and subsequent exhumation. Stress drops after a cataclastic event, as well as grain-size reduction by abrasion, may have activated dissolution-precipitation processes along cataclastic bands. Differential stress |s1-s3| increased as exhumation progressed after the cataclastic event. Estimates of paleostress based on calcite mechanical twinning indicate values of |s1-s3| >350 MPa during deformation. In contrast, mean flow stress during grain-boundary migration is estimated in s1-s3150 MPa. The high paleostress record and microstructures of the marble are consistent with the high exhumation rate calculated 110 MPa Ma-1. All of these data suggest that exhumation always occurred near the brittle-ductile regime of deformation.