Abstract
Principle sediment components are small-scale carbonate and mixed carbonate-siliclastic shallowing upward cycles arranged in laterally correlateable transgressive and highstand system tracts. As many as six third-order cycles are indicated over the studied time period. The Maracaibo platform drowned during the late Albian and was subsequently covered by cyclic pelagic limestones of the organic-rich La Luna Formation. -Authors
Original language | English (US) |
---|---|
Pages (from-to) | 25-33 |
Number of pages | 9 |
Journal | Unknown Journal |
State | Published - 1993 |
Externally published | Yes |
ASJC Scopus subject areas
- General Environmental Science
- General Earth and Planetary Sciences