This document discusses sedimentary rocks and how they provide clues about past environments. Sedimentary rocks form from the compaction and cementation of sediments like weathered minerals, chemical precipitates, and organic remains. Key clues used to interpret depositional environments include sediment size and shape, mineral composition, sedimentary structures like ripples and cross-bedding, fossils, color, geometry of rock units, and cyclical sequences indicating sea level changes. Together these clues can be used to map facies and reconstruct prehistoric landscapes through the principles of uniformitarianism and lateral continuity.
Sedimentary texture can be useful in interpreting the mechanisms and environment of deposition. It also has major control over the porosity and permeability of sediment.
Sedimentary texture can be useful in interpreting the mechanisms and environment of deposition. It also has major control over the porosity and permeability of sediment.
Komattite
Named after the Komati River in South Africa.
first described by Morris and Richard (twins) for ultramafic units in the Barberton Greenstone belt of South Africa.
Mostly of komatiite are Archean age
distributed in the Archaean shield areas.
Also a few are Proterozoic and Phanerozoic.
In all ages komatiites are highly magnesium.
Mostly a volcanic rock; occasionally intrusive.
Mafic rocks were identified as extrusive because of their volcanic textures and structures, and they seem to have been accepted as a normal component of Archean volcanic successions, Abitibi in Canada.
The ultramafic rocks were interpreted as intrusive which are founded as sills and dykes, Barberton in South Africa.
Spinifex texture-typical of Komatiites:
Structural geology is the study of the three-dimensional of the rock units with respect to their deformational histories, Structure is spatial and geometrical configuration of rock components.
Structures are classified into two types:
Primary structures.
Secondary structures
Primary structures
Structures that form during deposition or crystallization of the rock, are the result of two processes:
Settling of solid particles from fluid medium in which they have been suspended, in most of the sedimentary rocks.
Crystallization of mineral grains from a liquid in which they have been dissolved as in igneous rocks.
GEOLOGICAL THERMOMETERS
DEFINITION AND CLASSIFICATION
Proper understanding of origin of mineral deposits and their classification requires the knowledge of formation-temperatures of these deposits. Certain minerals, present over there, give information’s with regard to temperatures of their formations and of the enclosing deposits and they are known as geological thermometers. These geological thermometers may be classed chiefly into the following groups based on their preciseness:
1. The thermometers that record fairly accurately the specific temperature condition of formation of deposits.
2. The thermometers that provide an upper or a lower temperature, above or below which the deposits do not form
3. The thermometers that provide a range of temperature within which the deposits form; and
4. The thermometers that serve as rough indications of temperatures of formation of mineral deposits.
The presence of two or more of less precise geological thermometers in a deposit narrows the range of temperature of formation for the deposits
SOME OF THE MOST COMMON TEXTURES AND INTERGROWTHS OF IGNEOUS ROCKS, WHICH YOU SHOULD KNOW AS A PETROLOGIST.
ALSO, YOU WILL FIND PICTURES OF THE DESCRIBED CONTENT BOTH PETRO SECTION ALONG WITH THIN SECTION.
Komattite
Named after the Komati River in South Africa.
first described by Morris and Richard (twins) for ultramafic units in the Barberton Greenstone belt of South Africa.
Mostly of komatiite are Archean age
distributed in the Archaean shield areas.
Also a few are Proterozoic and Phanerozoic.
In all ages komatiites are highly magnesium.
Mostly a volcanic rock; occasionally intrusive.
Mafic rocks were identified as extrusive because of their volcanic textures and structures, and they seem to have been accepted as a normal component of Archean volcanic successions, Abitibi in Canada.
The ultramafic rocks were interpreted as intrusive which are founded as sills and dykes, Barberton in South Africa.
Spinifex texture-typical of Komatiites:
Structural geology is the study of the three-dimensional of the rock units with respect to their deformational histories, Structure is spatial and geometrical configuration of rock components.
Structures are classified into two types:
Primary structures.
Secondary structures
Primary structures
Structures that form during deposition or crystallization of the rock, are the result of two processes:
Settling of solid particles from fluid medium in which they have been suspended, in most of the sedimentary rocks.
Crystallization of mineral grains from a liquid in which they have been dissolved as in igneous rocks.
GEOLOGICAL THERMOMETERS
DEFINITION AND CLASSIFICATION
Proper understanding of origin of mineral deposits and their classification requires the knowledge of formation-temperatures of these deposits. Certain minerals, present over there, give information’s with regard to temperatures of their formations and of the enclosing deposits and they are known as geological thermometers. These geological thermometers may be classed chiefly into the following groups based on their preciseness:
1. The thermometers that record fairly accurately the specific temperature condition of formation of deposits.
2. The thermometers that provide an upper or a lower temperature, above or below which the deposits do not form
3. The thermometers that provide a range of temperature within which the deposits form; and
4. The thermometers that serve as rough indications of temperatures of formation of mineral deposits.
The presence of two or more of less precise geological thermometers in a deposit narrows the range of temperature of formation for the deposits
SOME OF THE MOST COMMON TEXTURES AND INTERGROWTHS OF IGNEOUS ROCKS, WHICH YOU SHOULD KNOW AS A PETROLOGIST.
ALSO, YOU WILL FIND PICTURES OF THE DESCRIBED CONTENT BOTH PETRO SECTION ALONG WITH THIN SECTION.
S6E5. Students will investigate the scientific view of how the earth’s surface is formed.
g. Describe how fossils show evidence of the changing surface and climate of the Earth.
c. Classify rocks by their process of formation.
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Session Overview
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4. Importance of Sedimentary Rx
1) Form 75% of exposed rx at
surface (outcrops)
- compose only 5% of total crust
2) Contain clues to reconstruct
past environments on Earth
11. Detrital Rock Process
1) Weathering
2) Erosion (transportation)
3) Deposition (sediment settles)
4) Lithification – turning sediment
into rock (“lithos” = rock)
(after sediment is buried)
12. Types of Lithification Processes
a) Compaction
- most effective on fine-grained rx
(ex: shale)
Exception: St. Peters Sandstone
Starved Rock State Park, IL
14. Sedimentary Rx Classification
2) Chemical – named based on
composition
Ex: calcite = limestone
halite = rock salt
plant remains = coal
15. Chemical Sedimentary Rocks
a) Inorganic – formed by chemical
reactions in environment
Ex: evaporites – rock gypsum,
rock salt
Ex: Travertine (limestone)
16. Inorganic Chemical Sed. Rx
Calcite:
*Limestone = mostly marine origin
Travertine = speleothems
Oolitic Limestone = tidal flats
* Most abundant chemical
sedimentary rock
30. Clues
3) Composition – minerals present
Two most common minerals found
in sedimentary rocks are _____
and ______ .
31. Variety of minerals:
Ex: quartz, K-spar, plagioclase
feldspar, mafic minerals, rock
fragments
- very little chemical weathering
- indicates rapid deposition close
to source area
Ex: arkose in alluvial fan
34. Sedimentary Structures
a) Bedding – layering w/in rock
Bedding plane – flat surfaces
along which rx tend to break or
separate
- separates different episodes of
deposition
35. Bedding
i) Laminar bedding – horizontal
layers
- usually deposited in calm energy
environment
Ex: shale, some sandstones
36. Bedding
ii) Graded bedding – sorted by
size
- occurs w/sudden decrease in
velocity
Ex: turbidity currents, alluvial fans
44. Clues
5) Fossils – evidence of
prehistoric life
Fossil record is incomplete
- shows remarkable pattern of
change from simple to complex
life forms
45. Steps to becoming a fossil
Step 1: Death
Step 2: Hard parts – bones, teeth,
shells (Who you are!)
Step 3: Rapid burial (Where you
die!)
Step 4: Time (prehistoric)
46. Fossils
Fossil record biased towards
marine environment
- abundant life in oceans
- many critters have hard parts
- lots of sediment for quick burial
52. Lithofacies map
For a particular moment in
geologic time, rocks indicate the
landscape
1) Map out the areas where each
rock type is found & draw
boundaries
53. Lithofacies map
2) Look at the lithologies (rock
types) & compare them to:
- nearby rx
- geometry of rock unit
3) Determine the original
depositional environment