Geologic Time - School of Earth Sciences


22 févr. 2014 (il y a 4 années et 4 mois)

132 vue(s)

Geologic Time

A: By correlating
stratigraphic records
worldwide, the Geologic
Column or Time Scale was
developed in the 19th century

(From: Murck and Skinner, 1999)

Q: How was this Earth
geologic history created?

Problems facing the Earth scientist:

Only partial information is available

Processes can only be observed as they are
acting now

Time scale for many processes much too long
to observe

Uniformity or Uniformitarianism:

natural laws are permanent: under the same
conditions a given cause will always produce the
same results

the present is the key to the past


opposing earlier view

Earth originated through supernatural means and
had been affected by a series of catastrophic
events such as the biblical Flood

Mudcracks in tidal flat

(From: Marshak, 2004)

Mudcracks preserved in Paleozoic siltstone bed

(From: Marshak, 2004)


the study of rock layers

and layering

borne sediments are deposited in horizontal
layers or strata

in any undisturbed sequence of layers, each layer
is younger than the layer below and older than the
layer above

a rock unit must always be older than any feature
that cuts or disrupts it

(From: Marshak, 2004)

Relative ages can be determined based on

three principles:

original horizontality

stratigraphic superposition

cutting relationships

Horizontal strata (~1 km thick) deposited on older strata that tilted and
deformed tectonically prior to deposition of the overlying strata

Absolute ages cannot be determined from

one stratigraphic record alone:

rates of sedimentation vary greatly

sediments are often compressed

gaps in the stratigraphic records

unconformity: boundary representing a gap

gaps may occur because sedimentation stopped
or because a layer was eroded


ll return to absolute ages a little later in the lecture.

(From: Marshak, 2004)

Siccar Point unconformity in Scotland

Movie 1 Geologic History

Q: What is the sequence of events that leads to these stratigraphic structures?

A: Watch the movie!

A: Correlating strata: the
fossil record

Rare fossilized fish

Species: Phareodus testis

Eocene Age

Kemmener, Wyoming

Complete fossilized articulated shrimp

Species: Carpopenaeus callirostris

Age: Late Cretaceous

Location: Hajoula, Lebanon

What is the role of fossils in determining
the Earth

s geologic history?

like swimming

Name: Keichousaurus

Age: Triassic

Formation: Huixia Beds

Location: Guanglin,
Guizhou Province, China

Beautiful Fossilized Dragonfly

Name: Aeschnidum cancellosa

Age: Late Jurassic to Early Cretaceous

Location: Beipiao, Liaoning


Sliced pyritized ammonite

Kosmoceras in Matrix

Upper Jurassic

Location: Ulyanovsk, Russia

Triple Kosmoceras in Matrix

Upper Jurassic

Location: Ulyanovsk, Russia

Correlating strata at three different locations; at location 3, stratum D is

Principle of fossil succession

(From: Marshak, 2004)

Fig. 10.12a

W. W. Norton

Fig. 10.12b

W. W. Norton

Fossil record restricted to the youngest eon, the

Precambrian: animals were soft
bodied and
fossils are imprints

Cambrian: appearance of animals with hard shells

Complete Trilobite in Matrix

Kanops raymondi



Q: Why is the stratigraphic
column mostly detailed for the
last one
tenth of Earth

geologic history?

A: See above 3 points.

Absolute age: the radioactive rock clock

Radioactivity: the process by which an element
transforms spontaneously into another isotope
of the same element or another element

Rate of decay is unaffected by changes in the
chemical or physical environment

Radiometric dating: use of naturally occurring
radioactive isotopes to determine the absolute
age of minerals or rocks

Absolute age: radiometric dating

radioactivity: transformation (decay) of an element
(parent) into another isotope of the same element
or another element (daughter)

the proportion of atoms that decays during each
time unit is constant

life: time needed for the number of parent
atoms to be reduced by one

once a mineral grain has formed, atoms are locked

by measuring the number of remaining parents
and the number of daughter atoms, the age when
the mineral was formed can be determined

Radioactive decay

Fig. 10.19

W. W. Norton

Using the rate of radioactive decay, the
absolute ages can be associated with the
stratigraphic column.



The movement of
plates throughout

Q: How were the Himalayan
Mountains and Tibetan Plateau

A: By the successive
accretions of various terrains to

Fig. 11.02 a, b

W. W. Norton