L13- Banded Iron Formations and other minerals

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25 Terms

1
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What do the Banded Iron Formations consists of?

Layers alternating with:

  • Magnetite (Fe3O4)

  • Hematite (Fe2O3)

  • Chert (SiO2)

2
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When is the oldest BIF?

Around 3.8 Ga

3
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Why are BIF’s important?

Major source of iron ore

4
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What event are BIF’s related to and what years did it last?

  • Great Oxidation Event (GOE)

  • 2.4-2Ga

  • O2 enters Earth’s system

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When were BIF’s abundant?

2.4-1.8 Ga

6
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When was there no dissolved Oxygen?

Archean Eon (4-2.5 Ga)

7
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What was sea water like in the Early Archean?

  • No O2

  • Rich in dissovled Fe 2+ and SiO2

8
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How did Fe 2+ enter the ocean?

  • Erosion of continents

  • Spreading ridges

9
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How is Fe 3+ made?

  • Oxidation of Fe2+ in seawater

  • Green Sulfur Bacteria

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What do the BIF represent?

  • seasonal temp fluctuations

  • Blooms of Green Sulfur Bacteria

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How is free O2 produced?

Through the first Cyanobacteria (Photosynthetic) in Stromatolites

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When were the first stromatolites?

Around 3.5 Ga

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Where is free O2 used

Used to oxidize Fe 2+ to form BIF bands

14
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At what time was there excess O2 that could escape to the atmosphere?

2.2 Ga - Cyanobacteria O2 oxidize all Fe

15
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What caused the production of BIF’s to stop?

  • Oxygenated surface waters extend into deeper water - Green Sulfur Bacteria like anoxic environments

  • Bacteria are pushed down where it is too dark to photosynthesize

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Why does pyrite begin to form?

  • sulfate (SO4 2-) produced is washed into the ocean

  • Sulfate-reducing bacteria in the deep ocean produce sulfide (H2S), which turns into pyrite (FeS2)

17
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in what form does sulfide accumulate?

in the form of pyrite (H2S)

18
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What are some characteristics of chert?

  • Conchoidal fracture

  • May occur as nodules or thick banded deposits

  • Formation is poorly understood

19
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What are some characteristics of Coal?

  • Concentration plant material - not oxidized

  • Volatiles driven off from coals

  • Very common in the Carboniferous of the Northern Hemisphere

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What are Volcaniclastic Sediments?

Clastic rocks composed mostly of volcanic materials that have been transported by wind and water.

21
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What are pyroclastic rocks?

Generated by explosive volcanic activity. Deposits include ash, lapilli, and bombs or blocks.

22
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What are Hyaloclastites?

  • Volcanic breccias containing a high proportion of black volcanic glass fragments.

23
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How do Hyaloclastites form?

When volcanic eruptions interact with water. Fragmentation formed by force or by thermal shock.

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What are Lahars?

Mudflow or debris flow containing a high proportion of volcanic debris.

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How are Lahars triggered?

  • Volcanic eruptions

  • Earthquakes

  • Wet conditions (Rainfall, or Melting of snow or glaciers)