PETROGRAPHY OF EXOTIC CLASTS IN THE SOEBI BLANCO FORMATION, BONAIRE, NETHERLANDS ANTILLES

The Paleocen e Soebi Blanco Formation in the island of Bonaire in Southeastern Caribbean has attracted the attention of geologists since 1931 when P. J. Pijpers pointed out the presence of a wide range of “foreign pebbles” in conglomerate beds. Interest was further boosted in 1986 with a Grenvillian...

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Main Authors: FRANCO URBANI, SEBASTIÁN GRANDE, JOSÉ MÉNDEZ BAAMONDE
Format: Article
Language:Spanish
Published: Universidad Nacional de Colombia 2013-01-01
Series:Boletín de Ciencias de la Tierra
Subjects:
Online Access:https://revistas.unal.edu.co/index.php/rbct/article/view/38759
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spelling doaj-b255579132404e069a454fbc04e9ea352020-11-24T20:43:40ZspaUniversidad Nacional de ColombiaBoletín de Ciencias de la Tierra0120-36302357-37402013-01-01033597033601PETROGRAPHY OF EXOTIC CLASTS IN THE SOEBI BLANCO FORMATION, BONAIRE, NETHERLANDS ANTILLESFRANCO URBANI0SEBASTIÁN GRANDE1JOSÉ MÉNDEZ BAAMONDE2Universidad Central de VenezuelaUniversidad Central de VenezuelaUniversidad Central de VenezuelaThe Paleocen e Soebi Blanco Formation in the island of Bonaire in Southeastern Caribbean has attracted the attention of geologists since 1931 when P. J. Pijpers pointed out the presence of a wide range of “foreign pebbles” in conglomerate beds. Interest was further boosted in 1986 with a Grenvillian age determined in a granulitic pebble (ca. 1150 Ma, U-Pb, TIMS, zircon) letting the authors propose an eastward translation of at least 300 km for the island of Bonaire relative to Guajira. New petrographic analysis of 21 rounded pebbles resulted in a wide span of rock types from metatrondhjemite, gneisses, metadiabase, andesitic lava and tuff, epiclastic metasedimentary, metapsamite, ultramylonitic marble, quartz arenite, conglomeratic sandstone and limestones (wackstonte, packstone). The variety of rock types support a combined arc-continental source region, a condition that was met in the northwestern corner of South America during Paleocene times.https://revistas.unal.edu.co/index.php/rbct/article/view/38759Conglomerateforeign pebblesPaleoceneEocene.
collection DOAJ
language Spanish
format Article
sources DOAJ
author FRANCO URBANI
SEBASTIÁN GRANDE
JOSÉ MÉNDEZ BAAMONDE
spellingShingle FRANCO URBANI
SEBASTIÁN GRANDE
JOSÉ MÉNDEZ BAAMONDE
PETROGRAPHY OF EXOTIC CLASTS IN THE SOEBI BLANCO FORMATION, BONAIRE, NETHERLANDS ANTILLES
Boletín de Ciencias de la Tierra
Conglomerate
foreign pebbles
Paleocene
Eocene.
author_facet FRANCO URBANI
SEBASTIÁN GRANDE
JOSÉ MÉNDEZ BAAMONDE
author_sort FRANCO URBANI
title PETROGRAPHY OF EXOTIC CLASTS IN THE SOEBI BLANCO FORMATION, BONAIRE, NETHERLANDS ANTILLES
title_short PETROGRAPHY OF EXOTIC CLASTS IN THE SOEBI BLANCO FORMATION, BONAIRE, NETHERLANDS ANTILLES
title_full PETROGRAPHY OF EXOTIC CLASTS IN THE SOEBI BLANCO FORMATION, BONAIRE, NETHERLANDS ANTILLES
title_fullStr PETROGRAPHY OF EXOTIC CLASTS IN THE SOEBI BLANCO FORMATION, BONAIRE, NETHERLANDS ANTILLES
title_full_unstemmed PETROGRAPHY OF EXOTIC CLASTS IN THE SOEBI BLANCO FORMATION, BONAIRE, NETHERLANDS ANTILLES
title_sort petrography of exotic clasts in the soebi blanco formation, bonaire, netherlands antilles
publisher Universidad Nacional de Colombia
series Boletín de Ciencias de la Tierra
issn 0120-3630
2357-3740
publishDate 2013-01-01
description The Paleocen e Soebi Blanco Formation in the island of Bonaire in Southeastern Caribbean has attracted the attention of geologists since 1931 when P. J. Pijpers pointed out the presence of a wide range of “foreign pebbles” in conglomerate beds. Interest was further boosted in 1986 with a Grenvillian age determined in a granulitic pebble (ca. 1150 Ma, U-Pb, TIMS, zircon) letting the authors propose an eastward translation of at least 300 km for the island of Bonaire relative to Guajira. New petrographic analysis of 21 rounded pebbles resulted in a wide span of rock types from metatrondhjemite, gneisses, metadiabase, andesitic lava and tuff, epiclastic metasedimentary, metapsamite, ultramylonitic marble, quartz arenite, conglomeratic sandstone and limestones (wackstonte, packstone). The variety of rock types support a combined arc-continental source region, a condition that was met in the northwestern corner of South America during Paleocene times.
topic Conglomerate
foreign pebbles
Paleocene
Eocene.
url https://revistas.unal.edu.co/index.php/rbct/article/view/38759
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AT sebastiangrande petrographyofexoticclastsinthesoebiblancoformationbonairenetherlandsantilles
AT josemendezbaamonde petrographyofexoticclastsinthesoebiblancoformationbonairenetherlandsantilles
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