SEDIMENTARY ARCHIVES Sedimentary Structures Sole marks.

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SEDIMENTARY ARCHIVES edimentary Structures ole marks
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Transcript of SEDIMENTARY ARCHIVES Sedimentary Structures Sole marks.

Page 1: SEDIMENTARY ARCHIVES Sedimentary Structures Sole marks.

SEDIMENTARY ARCHIVESSedimentary Structures

Sole marks

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SEDIMENTARY ARCHIVESSedimentary Structures

Flute casts

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SEDIMENTARY ARCHIVESSedimentary Structures

Tool marks

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SEDIMENTARY ARCHIVESSedimentary Structures

Flame Structures

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SEDIMENTARY ARCHIVESSedimentary Structures

Geopetal Structures or Which Way is UP?

Load structures

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SEDIMENTARY ARCHIVESSedimentary Structures

Geopetal Structures or Which Way is UP?

Mudcracks

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SEDIMENTARY ARCHIVESSedimentary Structures

Geopetal Structures or Which Way is UP?

Planar Cross-beds

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SEDIMENTARY ARCHIVESSedimentary Structures

Geopetal Structures or Which Way is UP?

Trough Cross-beds

Page 9: SEDIMENTARY ARCHIVES Sedimentary Structures Sole marks.

SEDIMENTARY ARCHIVESSedimentary Structures

Geopetal Structures or Which Way is UP?

Oscillation ripples

Page 10: SEDIMENTARY ARCHIVES Sedimentary Structures Sole marks.

SEDIMENTARY ARCHIVESSedimentary Structures

Geopetal Structures or Which Way is UP?

Tool marks

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SEDIMENTARY ARCHIVESSedimentary Structures

Geopetal Structures or Which Way is UP?

Fossils

Page 12: SEDIMENTARY ARCHIVES Sedimentary Structures Sole marks.

SEDIMENTARY ARCHIVESSedimentary Structures

Geopetal Structures or Which Way is UP?

Fossils

Page 13: SEDIMENTARY ARCHIVES Sedimentary Structures Sole marks.

SEDIMENTARY ARCHIVESSedimentary Structures

Geopetal Structures or Which Way is UP?

Raindrop Impressions

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SEDIMENTARY ARCHIVESInterpretation of Sedimentary Rocks

Provide information about conditions in and near the site of deposition

Such as: source area from compositionamount of transport erosion

Qtz vs. Feldspar (clay and ironcompounds) vs FerromagnesiansImmature vs mature

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SEDIMENTARY ARCHIVESClassification of Sedimentary Rocks

"Systems of classification are not hatracks, objectively presented to us by nature. They are dynamic theories developed to express particular views..."

Stephen Jay Gould

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SEDIMENTARY ARCHIVESClassification of Sedimentary Rocks

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SEDIMENTARY ARCHIVESClassification of Sedimentary Rocks

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SEDIMENTARY ARCHIVESClassification of Sedimentary Rocks

TEXTURE

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SEDIMENTARY ARCHIVESClassification of Sedimentary Rocks

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SEDIMENTARY ARCHIVESClassification of Sedimentary Rocks

Quartz Arenite

>90% Quartz

Cement: silica calcite

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SEDIMENTARY ARCHIVESClassification of Sedimentary Rocks

Feldspathic AreniteArkose

>25% Feldspar Granitic source Remainder is quartz

Cement: clay calcite iron oxides

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SEDIMENTARY ARCHIVESClassification of Sedimentary Rocks

Lithic AreniteGreywacke

>33% rock fragments Immature sandstone Poorly sorted, angular Remainder is quartz,

feldspar Cement: very little mostly clays

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SEDIMENTARY ARCHIVESClassification of Sedimentary Rocks

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CompositionCarbonate rocks consist of limestone and dolostone. The minerals present in each are: Limestone

Calcite Aragonite

Dolostone Dolomite

SEDIMENTARY ARCHIVESClassification of Sedimentary RocksCarbonates

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SEDIMENTARY ARCHIVESClassification of Sedimentary RocksCarbonates

Most of marine originDirectly or indirectly related to biological processes

Skeletal remains may be visibleCan be evaporites

Changes in water temp., alkalinity, CO2 conc.Clear, shallow tropical waters

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SEDIMENTARY ARCHIVESClassification of Sedimentary Rocks

Carbonates

Characteristics of most marine carbonate environments: Warm water Tropical climate (30 ° N - 30 ° S of equator) Shallow water (less than 200 m deep) Clear water (low to no terrigenous input) Sunlight required for photosynthesis by algae