In the Cretaceous melange of the Cordillera de la Costa belt, INTRODUCTION north–central Venezuela, there are knockers of eclogite, barroisiteTwo belts of high-pressure (HP)–low-temperature (LT) bearing eclogite, and pelitic glaucophane schist. These occur in a metamorphic rocks are exposed in the Caribbean Mounmetamorphic melange matrix that locally consists of marble, sertain system of northern Venezuela, which is part of the pentinite, amphibolite, actinolite schist, feldspathic schist and gneiss, complex east–west-trending boundary zone between the graphitic schist, chloritoid schist, and garnet-bearing mica schist. Caribbean and South American plates (e.g. Menendez, The protoliths for these various rock types exhibit a wide age range 1966, 1967). These two belts are the Cordillera de la (Cambrian to Early Cretaceous?). Recently discovered knockers of Costa and Villa de Cura belts, both of which were pelitic glaucophane schist contain Mg-glaucophane + paragonite metamorphosed during the mid-Cretaceous, presumably + kyanite + garnet + talc + graphite + rutile + quartz. in a subduction zone related to the mid-Cretaceous The coexistence of kyanite and Mg-glaucophane suggests minimum Leeward Antilles volcanic arc (e.g. Pindell, 1993). From P ~2000 MPa at T > 600°C. Eclogite knockers from the same Jurassic to Eocene time North and South America were outcrop contain garnet and clinopyroxene which yield ~500°C for diverging and new proto-Caribbean sea-floor was created cores, ~700°C for rims, and P [ 1200 MPa. The assemblage between them (e.g. Pindell, 1993). Therefore, the Leegarnet–biotite–phengite–albite within schists of the melange matrix ward Antilles arc, as well as the entire Caribbean Mounof this locality indicates metamorphic conditions of T = tain system, are allochthonous and formed far to the 450–520°C at P = 1800 MPa. Because all lithologies in this west as part of the Farallon–North/South American plate outcrop record high-P conditions, this metamorphic melange formed boundary zone (e.g. Pindell, 1993). before or during peak metamorphism in a mid-Cretaceous subduction Although the two HP–LT belts have similar metazone. morphic ages, they differ greatly in lithology and metamorphic history. The Cordillera de la Costa belt consists of oceanic and passive continental-margin rocks intermixed with Paleozoic granites and granitic gneisses. In this belt, the eclogites and blueschists were retrograded to epidote–amphiboliteand greenschist-facies assemblages following an apparent P–T path typical for
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