today: origin and interpretation of sedimentary rocks
DESCRIPTION
Sedimentary Rocks — Why Care? They are the repository of Earth’s history, especially the history of how the surface environment (including life) changed over time. To extract this history, we need to be able to “read” this rock record. They hold all of the oil, gas,coal, and water — locating these materials requires an understanding of the physical characteristics of different sedimentary rocks and how those characteristics change in 3-D.TRANSCRIPT
Today: Origin and Interpretation of Sedimentary Rocks
Wed: Origin and Interpretation of Metamorphic Rocks
Sedimentary Rocks — Why Care?
• They are the repository of Earth’s history, especially the
history of how the surface environment (including life)
changed over time. To extract this history, we need to be
able to “read” this rock record.
• They hold all of the oil, gas,coal, and water — locating
these materials requires an understanding of the
physical characteristics of different sedimentary rocks
and how those characteristics change in 3-D.
Coconino Sandstone
Coconino Sandstone up close
thin slice of Coconino sandstone seen through microscope
un-cemented quartz sand grains from a sand dune
So how are sedimentary rocks made?
Physical & Chemical Weathering → Sediment & Dissolved Ions
hincks146-147
Sedimentary Structures in the Coconino
This is the modern environment where large cross-beds form
Wind Direction
Fig. 5.21abc
W. W. NortonSo cross beds are tilted in the direction of flow (downstream)
Fig. 5.21d
Stephen Marshak
ripples
Stephen Marshak
Uniformitarianism — depositional environments of today are physically the same as ancient environments, so clues from the modern can be used to infer ancient environments from sedimentary rocks, or “the present is the key to the past”
Ancient ripples
Stephen Marshak
Mud cracks
Stephen Marhsak
Ancient mudcracks
Stephen Marhsak
Fig. 5.24c
© Martin Miller
Modern Alluvial Fan, Death Valley
Ancient Alluvial Fan Deposits
OOIDS (made of calcite — CaCO₃)imply shallow (<3m), tropical marine depositional environment
Ooids with cement, seen in a thin section, through a microscope
800 meters of oolitic limestones
Monte Bove in Italy
2 mm
So, the question is — how can we explain such a thick pile of shallow-water sediments?
We need to think about isostasy and sea level change in our search for an explanation of how we can get such thick piles of sediment, all of which appear to be deposited in fairly shallow water.
Isostasy
Isostasy
Equilibrium level for wooden block
time 1 time 4
time 1 time 4
So, the question remains — how to get such a thick pile of shallow-water sediments?
Add a WeightIncrease DensityThin CrustRaise Sea Level
As sea level goes down, previously deposited sediment will be eroded
In our case, crustal thinning makes sense because the
sediments in question were deposited during and after
continental rifting.
• Make sediment
• Transport & deposit sediment
• Create space to allow sediment to accumulate
• Compact and cement sediment
Depositional environments are interpreted based on studies of modern environments where sediment is deposited.
Summary on Making and Interpreting Sedimentary Rocks
Metamorphic rocks