Geology Test 3 Flashcards
Archean Eon
• Greenstone belts
• First evidence of life
• Chemical evidence
Hadean Eon
• Differentiation
• Origin of continental crust
Precambrian
Earth’s earliest time is referred
• Corresponding to all time prior to the Cambrian period (which contain conspicuous fossils).
• ~90% of geologic time.
• Rocks have fossils….just inconspicuous.
• Less than 20% of rocks at Earth’s surface are of Precambrian age.
Contains Hadean: 4.6-3.8 billion years ago
• Archean: 3.8-2.5 billion years ago
And Proterozoic eons
Hadean eon
In the Precambrian era
earliest interval of geologic time:
• Key points?
• Earth acquired it’s basic configuration
(mantle and crust surrounding the core).
• Insignificant amount of continental crust in
existence.
• Very few rocks of Hadean-Eon age exist today.
Archean eon
Second level in the Precambrian
second oldest interval of geologic time:
• Key points?
• First time when substantial continental
crust was formed.
• High heat flow from Earth’s interior was much greater than today….so continents remained small because they were constantly rifting apart.
Cratons
Precambrian rock:
large stable interior parts of continents that haven’t undergone substantial tectonic deformation in a long time.
• Edges of continents are sites of active orogeny
Precambrian Shield
Precambrian rock:
parts of the craton that are of Precambrian age.
• Canadian Shield is largest; exposed by erosion during recent glaciations
• Mostly Ig/Met; some have Sed rocks providing details about paleo-ecosystems.
Hadean Eon
• Early Earth was very hot due to:
• Impacts from asteroids and meteorites
• Radioactive decay
• Initial molten Earth was generally a homogeneously-mixed molten mass.
Atmosphere of hadeon eon
• Water vapor
• Hydrogen, carbon monoxide, carbon dioxide, nitrogen
• Methane (CH4) and ammonia (NH3)
• Little oxygen gas (O2)
What started first small
continental crust.
A much hotter early Earth melted subducted slabs of basalt to form
magma rich in Na (called granitoid; because richer in Na, not in K). Felsic crust formed by partial melting of oceanic lithosphere.
• Partial melting processes creates felsic magmas.
These felsic granitoids formed the nuclei of it
Tho Don’t have actual continental crustal rocks from Hadean.
Greenstone Belts
Part of Archean eon
Rock type
broad regions of elongate, stratified bodies consisting of high-grade metamorphic (felsic) rocks
• Have a distinct green color from metamorphic mineral, chlorite
• Formed by squeezing forearc basin sediments, deformed oceanic crust, and arc volcanics between margins of small protocontinents
2 major rock types of Archean eon
Greenstone belts
Banded iron formations
Banded Iron Formations (BIF)
• Typical of Archean sedimentary rocks
• Composed of alternations of iron-oxide-rich layers interbedded with chert layers:
• Chert + Fe-rich: precipitated from sea water
• Silica was more concentrated in ocean because this is before diatoms.
• Bacteria may have aided in precipitation of Fe
• The precipitation of iron does not occur in the oceans today.
Life first appeared on Earth sometime after…
4.5 Ga
Evidence for Archean Life:
Stromatolites
Still created today in association with Cyanobacteria (prokaryotic).
• Earliest known fossil life.