Evaporites Flashcards

Sed Rec

1
Q

What are Evaporites?

A

chemical sediments precipitated out of solutions by
evaporative concentration of dissolved salts

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2
Q

How many evaporite minerals are there?

A

More than 100

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3
Q

What are evaporates mostly made of?

A

Highly soluble ions (such as Na, Cl)

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4
Q

What are the main evaporite minerals?

A

gypsum, anhydrite, halite

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5
Q

What are the subordinate evaporite minerals?**

A

Mg & K salts, natron, and borax

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6
Q

TRUE OR FALSE

Some evaporite rocks are mono-mineral

A

TRUE! Examples are: gypsum, halite, etc.

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7
Q

Describe Halite

(chemical makeup, color, size, etc)

A

NaCl - cubic crystals (sometimes hooper-type),
granular, or massive colorless or white, sometimes
exotically colored

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8
Q

In evaporites, precipitation of halite leads to the developing
of:

A
  • Marine and non-marine evaporite deposits
  • Different colors depending on various lattice disorder or
  • presence of impurities (e.g., K+ gives a blue color)
  • Isotropic in thin section (as it is cubic), shows good
  • cleavage, and often fluid inclusions;
  • Hooper crystals (crater like): appear when a crystal grows
  • faster at the edges of each face than at the center
  • Happens when the growth is fast or/and not enough material to fill in the inner part
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9
Q

Describe Gypsum

(chemical makeup, color, size, etc)

A

CaSO 4 · 2H 2O - monoclinic; prismatic crystals or
aggregates when accumulates in massive beds

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10
Q

Describe Anhydrite

(chemical makeup, color, size, etc)

A

CaSO4 - orthorhombic, fibrous, massive, or nodular.
Colorless to pale blue or violet if transparent, white or brown if impurities are
present within crystal lattice Marine and non-marine evaporite

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11
Q

Where do Anhydrites form?

A

in restricted sub-aqueous and deep burial environments by dehydration
of gypsum at >22ºC mean annual temperature

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12
Q

TRUE OR FALSE

The texture of gypsum-anhydrite vary considerably

A

TRUE! Textures vary depending on their precipitation environment and diagenetic history

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13
Q

What does Gypsum look like under a cross polarized microscope?

A

weak birefringence and low relief

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14
Q

What does Anhydrite look like under a cross polarized microscope?

A

higher relief and moderate birefringence

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15
Q

Describe Trona

(chemical makeup, color, size, etc)

A

Na3(HCO 3)(CO 3)· 2H 2O - monoclinic, forming well-developed columnar and fibrous crystals or massive aggregates

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16
Q

Is Trona marine or non-marine and when is it deposited?

A
  • Non-marine evaporite
  • Deposited in the latest stage of a salt lake evolution
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17
Q

Trona is mined as the primary source of _?

A

Sodium Carbonate

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18
Q

What are some uses of Trona?

A
  • manufacturing of glass, paper, detergents, and food additive
  • fertilizer (potash)
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19
Q

Describe Borax

(chemical makeup, color, size, etc)

A

hydrous sodium borate Na2B 4 O 5 (OH) 4 · 8H 2O - monoclinic, forming well-developed prismatic crystals or earthy aggregates

20
Q

Is Borax marine or nonmarine and what are some uses of it?

A
  • Non-marine
  • Used for detergent, cosmetics, enamel
21
Q

Depositional Environments

Evaporite deposits are commonly

A

cyclic

22
Q

How many modern sites of evaporite precipitation are there?

A

Few and none of them scale to what existed in the past

23
Q

What are the 5 different environments (see figure at right) in which
deposition of evaporites take place in?

A
  • Marine: deep (shabka/lake/lagoon; 1-2-3)
  • Shallow water (intracratonic/rift basin; 4)
  • Non-marine: takes place within sediment (sabkha;2) or in very shallow to desiccated saline pans (5)
    Has taken place on the floor of deep-marine basins following evaporative drawdown and extreme desiccation
    EX: Mediterranean basin
24
Q

What does Sabkha mean?

A

Salt flat (arabic)

25
Q

What is the most common precipitate in sabkhas?

A

Gypsum

26
Q

Describe Sabkha

(location, regions, etc)

A
  • Extensive, barren (not necessary), salt-encrusted, and periodically flooded
  • Coastal and inland mudflats in arid regions
  • Broad coastal intertidal and supra tidal
27
Q

What are crystal forms found in sabkhas?

A
  • Desert roses
  • Selenite
  • Twinned crystals
28
Q

When gypsum crystal are replaced by anhydrite (high evaporation) then:

(what textures form)

A

chicken-wire & enterolithic textures form

29
Q

Sabkha

Precipitation of evaporites happens within the sediment from pore waters derived from:

A

seawater/groundwater recharge and seawater flood recharge

30
Q

Sabkha Cyclicity

Cyclicity is common in sabkha evaporite sequences; it is controlled by

A

sea-level changes

31
Q

Sabkha Cyclicity

Typical facies are:

A

nodular (chicken-wire) and enterolithic anhydrite

32
Q

Sabkha Cyclicity

What are key features to identify?

A
  • shallow water and intertidal sedimentary
  • structures contained within associated carbonates
33
Q

Sabkha Cyclicity

What are examples of modern sabkha environments?

A
  • Trucial Coast of the Arabian Gulf
  • Texas
  • Southern Mediterranean coast of Tunisia
  • Egypt
34
Q

Sabkha Cyclicity

What are examples of ancient sabkha environments?

(of permian age)

A

Delaware Basin of Texas and New Mexico

35
Q

What are Marine Deep Evaporites?

A

The “deeper” version of the barred basins

36
Q

Late Miocene evaporites from the Mediterranean Basin were erroniouslly interpreted as?

and the gypsum deposits can reach a thickness of what?

A
  • deep water/subaerieal in origin
  • > 2km thick
37
Q

Non-Marine: Sabkha

A
  • Continental sabkha is the part of a playa mudflat complex
    • Brine seepage ascends through capillary action
  • Atacama Desert is the driest place on Earth
38
Q

Non-Marine: Saline Lakes

Non-Marine: Saline Lakes Develop where?

A

arid and semi-arid regions
* Modern ephemeral and perennial saline lakes/seas occur in many desert
areas:
* Great Salt Lake (UT), Mono Lake (CA), and Dead Sea (Israel)

39
Q

Non-Marine: Saline Lakes

What do the evaporite precipitation look like?

A

a bull’s eye pattern

40
Q

Non-Marine: Saline Lakes

Modern ephemeral and perennial saline lakes/seas occur in many desert areas such as:

A
  • Great Salt Lake (UT)
  • Mono Lake (CA)
  • Dead Sea (Israel)
41
Q

Non-Marine: Caves

Where are Non-Marine Caves found?

A
  • Lechuguilla, Carlsbad Caverns (NM)
  • Naica (Mexico)
  • Frasassi (Italy)
  • Mammoth (KY)
  • Pulpi (Spain)
42
Q

Non-Marine: Caves

What morphologies are found in this environment?

A

Unspectacular rafts, flowers, and crystals (mm to
meters) from vapor phase precipitation

43
Q

Salt Domes

Halite is ductile and:

A
  • Flows when tectonically stressed during burial
  • Massive halite beds can undergo plastic deformation  salt domes (aka diapirs)
44
Q

TRUE OR FALSE

Salt Domes can influence surface topography and litho-stratigraphy

A

TRUE! This process is referred to as salt tectonics.

45
Q

Salt Domes

Truncated layers punctured by the rising salt form:

A

Perfect oil traps. Bouyant oil trapped beneath impermeable salt