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Inset box 4: propeller fault projected into cross section XY (grey in main figure), showing possible pathway for some of the subducted material. Contiene: Bocca Dorata e il segreto di Tristan Bantam - Appuntamento a Bahia - Samba con Tiro Fisso. Subsequent closure of the Andean Back-Arc Basin resulted in accretion of Caribbean terranes to western Colombia. A fault zone containing a large elongate body of serpentinized peridotite separates the two metamorphosed units.

As a consequence of the development of the Yucatan Basin in the western part of the orogenic belt, the Pinos, Escambray, and probably the Guayabal terranes were exhumed in an intra-arc environment, whereas the East Yucatan(?

Inset box 2: onset of SW-dipping subduction at backthrusts, with HP/LT rocks already in hanging wall. During mid-late Cretaceous time, the Caribbean arc (also known as the Protoantillean arc) migrated to the northeast and east, probably with a strong axis-parallel stretching component due to the sinistral oblique subduction of the Proto-Caribbean lithosphere.

Mafic rocks appear as variably sized tectonic blocks within serpentinite that underwent variable alteration at low pressure. The sequence began with the extrusion of various volcanic types that constitute the Los Ranchos Formation. In 1967, Pratt met Florenzo Ivaldi; the two created a comics magazine named after his character, Il Sergente Kirk, the hero first written by Héctor Oesterheld. Many of the minor characters cross over into other stories in a way that places all of Pratt’s stories into the same continuum. La infiltración de estas salmueras a través de la potente secuencia de areniscas y limolitas aumentó su temperatura hasta 100-200ºC favoreciendo la disolución y movilización del Zn y Pb necesarios para formar la mineralización principal.

La etapa de fracturación/brechificación facilitó también el ascenso de fluidos reductores equilibrados con los niveles de pizarras negras intercalados en la secuencia siliciclástica, que aportaron Au y Ba a la mineralización. The Proto-Caribbean basin (related to the Central Atlantic) formed in between the Americas during Jurassic-late Cretaceous time and started westerly-directed subduction below the Pacific (Farallon plate) in the early Cretaceous, forming backarc, forearc and arc settings in the leading edge of the Caribbean plate (Boschman et al. The tectono-metamorphic event dated here overlaps with the inception of Turonian-Coniacian SW-dipping subduction and metamorphic sole formation in a back-arc position recorded in the Moa-Baracoa ophiolite complex in neighboring Eastern Cuba.