Introduction Flashcards
Tectonics
structure and tectonics interact, cant draw a line between them
tectonics are external processes that cause a characteristic set of structures in an area
plate tectonics
salt tectonics
neotectonics
- crustal motions and contemporaneous stress field
plate tectonics
- movement and interaction of lithospheric plates
there are major and smaller plates
plate boundaries join to form a network
example of subduction ->indian plate started to collide with Asia about 15 million years ago
salt tectonics
salt is a rock
- deformation from vertical movement of salt through its overburden
-layers of salt cut through the sedimentary layers above them
-salt is not permeable
deformation
conglomerate (large clasts, matrix supported) -> clasts can get flattened or stretched
different rocks behave differently under the same conditions
->not all rocks deform in the same way under the same chemical an physical conditions
the same rock will behave differently depending on the chemical and physical conditions (HPT vs LPT)
usually high pressure and high temperature go together ->not always
stress
stress on a plane is the force per unit area of the plane
stress = force/area
the same force applied on a smaller area will cause more damage
deformation and strain
any change in shape/distortion (strain), position (translation), or orientation (rotation) of a body under stress
3 components: rotation, translation, and strain
as long as a rock has one of three components, you can say it is deformed
homogeneous vs inhomogeneous (heterogeneous)
homogeneous -> everything has moved/been changed in the same way
factors that affect deformation
different rock types (chemical/mineralogical composition)
->have different chemical properties
physical and chemical environments
main types of structures
Non-tectonic (primary)
->not due to deforming forces
->formed during the formation of the rock
Tectonic (secondary)
1. Brittle structures
2. Ductile structures
types of tectonic structures
brittle -> loss of cohesion
ductile -> no loss of cohesion
scale of observations
microscopic
-> only visible under thin section
mesoscopic
-> can be observed directly
-> from hand samples to large, continuous outcrop
macroscopic
-> several outcrops to whole mountain ranges
-> cant be observed directly, need interpretation
methods in structural geology
fieldwork - most essential
other techniques - data and modelling, measuring crystallographic orientation of constituent crystals, look at structural details within individual crystals
structural analysis
2 distinct steps:
- study and description of a rock in its present state
2.
geometric analysis
geometrical features are studied
infer what the geometry is, descriptive, free from reference
characterization of the form, extent, and arrangement of structures in a map area
kinematic analysis
from the results of the geometrical analysis
-> attempt to reconstruct movements that took place during the deformation of the rock
-> rotation, translation, strain
how the geometric formed