Green River iaminites: does the playa-lake model really invalidate the stratified-lake model
Journal Article
·
· Geology; (United States)
OSTI ID:6766263
Proponents of the playa-lake model have proposed deposition of most of the Green River Formation microlaminated carbonates (including oil shales) in lakes that were not perennially stratified (meromictic). However, there is a variety of evidence favoring a meromictic depositional environment: (1) close similarity of much of the lamination to varves in modern meromictic lakes, (2) evidence that hydrologic events favoring development of meromixis (chemical stratification) occurred prior to deposition of major accumulations of oil shale, (3) mutually exclusive distribution of fossil nekton (especially fish) and normal lacustrine benthos (including mollusks), and (4) analogy with a Quaternary playa that became a meromictic lake following increased inflow. The playa-lake model is untenable for the typical fish-bearing, kerogen-rich microlaminated sediments. These laminites were probably deposited in a large ectogenic meromictic lake - a chemically stratified lake that formed when increased fresh-water inflow ''drowned'' a saline playa complex.
- OSTI ID:
- 6766263
- Journal Information:
- Geology; (United States), Journal Name: Geology; (United States) Vol. 10:6; ISSN GLGYB
- Country of Publication:
- United States
- Language:
- English
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