Carbonate Environments Flashcards
(43 cards)
For Dunham’s grainstones, would you find them below or above wave base?
Above. there is no mud
For Dunham’s mudtsones, are they high or low energy?
low
What would cause a buildup of carbonate material?
- need a lot of organisms with carbonate skeletal structures
- low siliclastic input, need a flatter terrain so sediment doesn’t come down from the continent
What is a sabkha?
A transition zone where the environment goes form wet to dry. It is an area of high evaporation, so get a lot of evaporites.
What type of environment do you usually find carbonates?
Tropical
What is a shoal?
Ribbed, ramp like underwater sandbar that is slightly off shore. Between a shoal and the shore is a lagoon.
Describe Irwin’s Z Zone
The area of water closest to the shore - includes lagoons, tidal flats and sabkha. Low energy. You get algal laminations, stromolites, burrowing and desiccation cracks. You also get fecal pellets (bc there isn’t much aggitation disturbing the seds), intraclasts, skeletal sands and mud.
T/F: In order to make carbonates, you need very deep & turbid water.
F, you need clean and shallow water.
Describe Irwin’s Y Zone
The area where you see a shoal, high energy area. Tidal megaripples, barrier islands and reefs. The structures you would get are: cross-bedding, cross-lamination and channeling. You would also see oolitic and skeletal sands, and reefs.
Describe Irwin’s X Zone
You would throw your ex here.
Offshore, low energy. You would get lamination in this area. Mostly mud lithology.
Where, in Irwin’s sedimentation model, would you get wackestones, packstones, grainstones and mudstones?
X Zone - mudtsones
Y Zone - wackestone & packstone at edges of shoal. grainstone at highest point of shoal
Z Zone - wackestone
Where does wave base begin in Irwin’s sedimentation model?
X zone
Study Irwin’s XYZ vertical sequence
Study this carbonate shelf diagram showing where you can find diff lithologies and grain types on carbonate shelfs
What are grape stones and where do you usually find them?
Grapestones are an aggregate of carbonate grains. You usually find them below wave base. Commonly found in shallow, low-energy environments like subtidal areas, where carbonate grains are subjected to less intense wave action.
What are ooids? Where are they found in carbonate shelf environments?
carbonate grains that consist of concentric layers of calcium carbonate precipitated around a central nucleus. found in the slope of a carbonate shelf
If you see ooilitic shoals, what does that tell you about precipitation rate and amount of agitation happening?
It is high precipitation and high agitation
What are the components that go into making lime mud on lagoon floors?
pellets, break up of larger carbonate grains, bio-erosion, death of algea, erosion of tidal flats
How does sea level change affect carbonate shelves?
In a high sea level time the sediment is deposited because the floor is below wave base, but in low sea level there is an erosion and lithification of the floor
What is a reef?
A structure on the floor created by living organisms. The kind of organisms that contribute to a reef change over time.
Study this diagram about reef sections
What is the highest point on a reef called?
The reef crest. Shallow corals encrusting and hemispherical corals, high energy
This slide is on the exam - study
Review Dunham classification