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 - Jan 1 1993 |
ASJC Scopus subject areas
- Environmental Science(all)
- Earth and Planetary Sciences(all)