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Carbonate Ramp Facies.

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Presentation on theme: "Carbonate Ramp Facies."— Presentation transcript:

1 Carbonate Ramp Facies

2 Carbonate Ramps Consistent shallow gradient from shoreline to basin (some may be distally steepened), somewhat analogous to siliciclastic shelf Highest Energy Lowest Energy

3 Carbonate Ramp Environments
Deep ramp Mid ramp Inner ramp Peritidal Offshore Deep Subtidal Shallow Subtidal Offshore- Transition Offshore Shoreface Siliciclastic Equivalents

4 Thin packstone “tempestites” in lime mudstone (or siliciclastic mud)
May be normally graded or contain HCS; gutter casts/sole marks on base Deep Subtidal, Offshore Offshore Deep Subtidal

5 Large subaqueous dunes, generating large-scale cross-bedding
Shoals (ooids or skeletal) are much more common than in clastic settings Large subaqueous dunes, generating large-scale cross-bedding Shallow Subtidal

6 Other sedimentary structures and facies may be similar to siliciclastics (wave ripples, SCS, low-angle parallel beach laminations, etc.) Swaley cross-stratification (SCS) Beach deposits Low-angle beds with hardgrounds

7 Peritidal Carbonates

8 Typical facies: light gray or light brown limestone/dolostone with
Crinkly or wavy lamination from microbial mats Fenestrae: mm-sized voids (sometimes filled by calcite spar) formed by trapped gas bubbles or beneath microbial mats

9 Polygonal desiccation cracks (wedge shaped in side view) formed by drying and thermal contraction during tidal cycle

10 Tepee Structures in high intertidal/supratidal zone

11 Continued cycles of desiccation disrupt tepees, forming flat pebble conglomerates

12 CAUTION: flat-pebble conglomerates occur in any place where thin layers of limestone are subject to seafloor lithification (e.g., also in wave-influenced beaches and in many subtidal environments before the Ordovician)

13 (or pseudomorphs after gypsum)
Supratidal sabkha environments (arid supratidal flats) characterized by evaporite mineral (gypsum, anhydrite, rarely halite) formation Gypsum laths (or pseudomorphs after gypsum) Anhydrite nodules

14 Classic carbonate platform environments
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