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Geology: Sedimentary Rocks Formation and Tectonic Processes, Summaries of Geology

The formation of sedimentary rocks through sediment deposition and the impact of tectonic processes such as uplift and erosion. Topics include original horizontality, superposition, cross-cutting relationship, and different types of faults and unconformities.

What you will learn

  • What are the primary factors in the formation of sedimentary rocks?
  • How do tectonic processes affect sedimentary rocks?
  • What are the different types of faults and unconformities mentioned in the document?

Typology: Summaries

2021/2022

Uploaded on 09/12/2022

gaurishaknar
gaurishaknar 🇺🇸

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uplift
erosion
sediment deposited more sediment deposited more sediment deposited more sediment deposited
sediment deposited more sediment deposited and
lithified to form sedimentary rock
rocks deformed by tectonic stress rocks uplifted and eroded
sediment deposited
and lithified
Later, clasts derived from the lower unit
are included in the next later of sediment
Any rock in the
Earth’s crust
Magma intrudes, picking up inclusions
from the surrounding rock, then cools to
form igneous rocks with inclusions
Almost all sedimentary rocks formed from deposits of sediment at the surface of the Earth. Once a sedimentary
bed has been deposited, new sediment settles on top of it. Thus, in undisturbed strata, the oldest sedimentary
rocks will be on the bottom of the stack. Applies only to sedimentary rocks and some volcanic rocks.
Almost all sedimentary rocks formed from basically horizontal deposits of sediment. Thus any sedimentary rock
unit that is no longer parallel to the Earth’s surface had be have been deformed (tilted or folded) after it was
lithified. Applies only to sedimentary rocks and some volcanic rocks.
Some rocks contain broken pieces of other rocks (called inclusions or clasts). The rock that supplied the inclu-
sions must have already existed at the time the rock containing the inclusions formed. Thus, the included rock is
from an older rock. Applies primarily to igneous intrusions and sedimentary rocks.
Inclusion
Original Horizontality
Superposition
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uplift

erosion

sediment deposited more sediment deposited more sediment deposited more sediment deposited

sediment deposited more sediment deposited and lithified to form sedimentary rock

rocks deformed by tectonic stress rocks uplifted and eroded

sediment deposited and lithified

Later, clasts derived from the lower unit are included in the next later of sediment

Any rock in the Earth’s crust

Magma intrudes, picking up inclusions from the surrounding rock, then cools to form igneous rocks with inclusions

Almost all sedimentary rocks formed from deposits of sediment at the surface of the Earth. Once a sedimentary

bed has been deposited, new sediment settles on top of it. Thus, in undisturbed strata, the oldest sedimentary

rocks will be on the bottom of the stack. Applies only to sedimentary rocks and some volcanic rocks.

Almost all sedimentary rocks formed from basically horizontal deposits of sediment. Thus any sedimentary rock

unit that is no longer parallel to the Earth’s surface had be have been deformed (tilted or folded) after it was

lithified. Applies only to sedimentary rocks and some volcanic rocks.

Some rocks contain broken pieces of other rocks (called inclusions or clasts). The rock that supplied the inclu-

sions must have already existed at the time the rock containing the inclusions formed. Thus, the included rock is

from an older rock. Applies primarily to igneous intrusions and sedimentary rocks.

Inclusion

Original Horizontality

Superposition

Cross-Cutting Relationship

Some geological events (e.g., erosion, igneous intrusion and faulting) can cut across and partially obliterate other

structures. The feature that is cut must have already existed when the cutting event. Thus the feature that cuts is

younger than the feature(s) that is cut. ONLY applies faults, intrusions and unconformities.

undisturbed rocks tectonic stress causes the rock to fracture and shoves the upper block up over the lower block

reverse fault

Faults

Unconformities

sediment deposited

sediment deposition stops. Time passes. New sediment may be deposited, but is eroded away.

sediment deposition begins again. The contact betwen the sedimentary units is a disconformity

sediment deposited and lithified to form sedimentary rocks and buried

rocks tilted by tectonic stress, uplifted to the surface and eroded

new sediment deposited on top of erosional surface, forming and angular unconformity.

disconformity

angular unconformity

metamorphic and/or igneous rock forms deep within the Earth

Rock units uplifted to the surface of the Earth and eroded

uplift

erosion

uplift

erosion

nonconformity

Sediment deposited on non-conformity

tectonic stress causes the rock to fracture and lower block slides down relative to upper block

normal fault

OR