Archean Flashcards
(30 cards)
3 Reasons why there are no rocks older than 4.0 billion years old?
a.) many of the rocks have been metamorphosed
b.) deeply buried beneath younger rocks
c.) contain few fossils of any use in biostratigraphy
5 Events during the Archean Eom
Differentiation of the Earth’s Layers
Formation of the Atmosphere
Formation of the Ocean
Formation of the Continents
Earth’s Earliest Organisms
2 principal divisions of Earth’s surface
continents
ocean basins
percent of Earth’s human population that lives on the continents
95%
Earth’s first crust was probably?
Basalt
Mineral that is 4.4 billion years old indicating that source rocks that old must have existed.
Zircons
is not defined by its size, location, who discovered it, or whether it is surrounded by oceans. Rather, it is defined by the rocks it’s made of and how it came to be that matter.
Continent
2 Major Features of the Continents
Stable Interiors
Mountain Belts
extensive, flat stable areas that have been eroded nearly to sea level
Stable Interiors
uplifted regions of deformed rocks
Mountain Belts
expansive, flat regions composed of deformed crystalline rock
Shields
Other flat areas of the stable interior in which highly deformed rocks, like those found in the shields, are covered by a relatively thin veneer of sedimentary rocks.
Stable Platforms
the formation of large crustal provinces that, in turn, accreted with others to form even larger crustal blocks called?
Cratons
The portion of a modern craton that is exposed at the surface.
Shield
% of Earth’s exposed Precambrian crust is Archean
22
2 most common variety of rocks in the Archean crust
greenstone
granite-gneiss complexes
are actually composed of a variety of rocks, with granitic gneiss and granitic plutonic rocks being the most common, that were probably derived from plutons emplaced in volcanic island arcs.
Granite-gneiss complexes
are subordinate, accounting for only 10% of Archean rocks, and yet they are important in unraveling some of the complexities of Archean tectonic events.
Greenstone belts
Greenstone belts typically have what kind of structure?
synclinal structure
The most interesting igneous rocks in greenstone belts
Komatiites
Reason why komatiite can no longer be produced
ultramafic flows no longer occured
theorized to be Earth’s first supercontinent, beginning its formation about 3.6 Ga (billion years ago), completing its formation by about 3.1 Ga and breaking up by 2.5 Ga.
Vaalbara
supercontinent, existence of which is also only supposed, formed approximately three billion years ago.
Ur