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Marginal-Marine Environments

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Presentation on theme: "Marginal-Marine Environments"— Presentation transcript:

1 Marginal-Marine Environments
Deltas, Beach and Barrier Island systems,

2 Marginal Marine Transitional Where land meets the sea
Dominated by rivers (fluvial), wave, and tidal processes. High-energy – waves and currents Quiet water – lagoonal, and estuarine

3 Deltas – Deltaic system
Alluvial Delta Subaerial, subaqueous Sediment in a standing body of water

4 Ancient Delta Deposits
Found in all ages of stratigraphic sequences Important petroleum and natural gas deposits, coal, and other mineral resources, uranium is one. Excellent reservoir rocks, cap rocks and traps in this sequence of rocks, stratigraphic traps

5 Modern deltas Table 9.1 Largest delta plain area = Ganges –Bramaputra
Large water discharge = G-P, Irrawaddy, Mississippi

6 Classification of Deltas

7 Delta Classification 2 Figure 9.3

8 Cross-Section of a Delta
progradation

9 Delta formation

10 Cross-section Gilbert-type deltas, in your book, Figure 9.4

11 Figure 9.12 Components of a Delta

12 Sediment Characteristics of Deltas
Deltaic plain – subaerial component Subaqueous Deltaic plaine Delta front prodelta

13 Closer view of the cross-section

14 Flow and Discharge Jet – discharge of sediment
Homopycnal flow – equal density water of river entering basin of equal density water, rapid mixing and abrupt deposition of sediment. Hyperpycnal flow – river water higher density than basin water, flows beneath the basin water, vertically oriented plane-jet flow, forms turbidites on gentle slope of delta. Hypopycnal flow – river water is less dense than the basin water, river flow into marine or saline lake flow on top of basin as a horizontal plane-jet,

15 Bird-foot Delta

16 History of the Mississippi Delta

17 River-Dominated Delta

18 Wave-dominated Delta

19 Tidal-dominated Delta

20 Fan Delta Figure 9.11

21 Delta Cycles Transgression of sea
Progradation of delta seaward – construction phase Coarsening-upward sequence Fine prodelta muds overlain by delta front silt and sand Distributary-mouth sands on top of these Marsh and fluvial deposits Transgression of sea Destruction phase

22 River – Dominated Strata

23 Wave-dominated delta Strata

24 Tide-dominated delta strata

25 Ancient Delta system - Mississippian
What tectonic event would these deltas be associated with of the Appalachian Mountains?

26 What do you know of the sea?
Ocean currents? Rotation? Hurricanes rotate in what direction? What about tides? How many low tides per day? Spring tide? Neap tide?

27 Surface Currents

28 Spring Tide and Neap Tide

29 Beach and Barrier Island Systems
Beach is the dominant marginal marine deposit What is the dominant Wentworth’s clast size found on the beach?

30 Depositional Settings
Tidal ranges Microtidal = 0 – 2 m tidal range, barrier islands Mesotidal = 2 – 4 m tidal range Macrotidal = > 4 m tidal range

31 Beach to Barrier Island
Single Beach – attached to the mainland Strand Plain – broad beach-ridge system, multiple parallel beach ridges and parallel swales, lack well-developed lagoons or marshes Chenier Plain – sandy ridges elongated along the coast and separated by coastal mudflat Barrier Island – separated wholly or partly form mainland by a lagoon or marsh

32 Beach Littoral zone

33 Breakers

34 Longshore Current

35 Rip Current

36 Prograding Beach Figure 9.25

37 Barrier Islands and Lagoon

38 Barrier Island Figure 9.23

39 Characteristics Beach deposits Backshore Shoreface deposits
Fine to medium Sand Heavy-mineral laminae Backshore Eolian sand deposits Storm-wave deposits Shoreface deposits Upper shoreface – bidirectional cross-bedding sets, Skolithos burrows, Middle shoreface – fine to medium sand, shell material, landward and seaward dipping cross-beds, Skolithos and ophiomorpha Lower shoreface – fine to very fine sand, intercalated layers of silt and mud, small scale cross-stratification, horizontal laminations, hummocky cross-stratification

40 Deposits Back-barrier
Washover deposits – sandy deposits in the mud-rich lagoon Tidal-channel deposits – sand and lag deposits, fluvial marine deposit, cross-bedding Tidal delta deposits – sandy deposits, parabolic shape in cross-section Tidal Flat deposits – sand lenses and mud deposit Lagoonal – fine grained muds, organic rich muds Marsh – sandy to silts to muds, peat deposits, bioturbated a lot.

41 Barrier Islands Figure 9.26

42 Galveston Island

43 Delaware Island

44 Barrier Island Sequence

45 Back-Barrier Figure 9.27

46 Pennsylvanian Lagoon

47 Barrier Island and Lagoon - Estuary

48 Estuary


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