Abstract
The largely phyllitic Tucutunemo Formation of the Caribbean Mountains of N-central Venezuela has been assigned to the Early or Late Cretaceous on the basis of lithologic correlation. Reexamination of some limestones in thin section revealed a crinoid-brachiopod microfacies in which productid spine bases and sections were identified. Other forms include bryozoans, probable dasyclad algae, and a possible chaetetid. The microfacies closely resemble those of limestones of the Permian Palmarito Formation of the Venezuelan Andes. These features suggest a (late?) Paleozoic age for the Tucutunemo Formation. A range of possible tectonic settings for the formation is summarized in 2 autochthonous and 2 allochthonous models. -Authors
Original language | English |
---|---|
Pages (from-to) | 922-926 |
Number of pages | 5 |
Journal | Geology |
Volume | 15 |
Issue number | 10 |
DOIs | |
State | Published - 1 Jan 1987 |
ASJC Scopus subject areas
- Geology