IGNEOUS PETROLOGY (BASALT) Flashcards

1
Q

Etymology of Basalt

A

Basaltes - misspelling of basanites
Basanites - very hard stone
Basanos-touchstone
Bauhun - Slate

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2
Q

Composition of Basalt

A

45-52% SiO2
Ca- Plag
Augite -CaPyx
Alkali <5%

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3
Q

3 Principal Basalt Types and their Environment of Formation

A

1) Tholeiitic - MOR and Ocean Island (Hotspots)
2) Alkali - Ocean Islands and Continental Rifts
3) Calc Alkaline - Convergent Plate Boundaries

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4
Q

Groundmass
Tholeiitic vs Alkali

A

Tholeiitic Basalt
?Fine grained
?No Olivine
?Cpx - Augite and/or Pigeonite
?Opx Hypersthene may rim Olviine
?No Alkali Feldspar
?Intersitital Glass

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5
Q

Phenocrysts
Tholeiitic vs Alkali Basalt

A

?Unzoned Olivine sometimes w/ Opx rim
?Opx uncommon
?Early Plag Common
?Cpx Pale Brown Augite

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6
Q

Basalt used in place of Nepheline Olivine Basalt

A

Alkali Basalt

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7
Q

Basalt containing olivine

A

Olivine Phyric Basalt

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8
Q

Basalt visibly enriched in olivine crystals ofte as phenocrysts

A

Picrite

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9
Q

Basalt with Olivine and Augite (Cpx) Phenocrysts which may have been enhanced due to gravitational accumulation

A

Ankaremite

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10
Q

Rocks that have lower SiO2 than Basalt and in the lower left of TAS <45% SiO2 and more olivine-rich and contain little plagioclaise

A

PicroBasalt

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11
Q

Have Mafic Mineral similar to basalt but contain plag of more sodic composition and silca of 52-57%

A

Basaltic Andesite

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12
Q

Basalts which recognizable alkali feldspars or feldsphathoids

A

Trachybasalt
Basanites (>10% Ol)
Tephrites (<10% Ol)

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13
Q

Trachybasalt that has Na>K content

A

Hawaiite

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14
Q

Trachybasalt that has Na

A

Potassic Trachybasalt

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15
Q

High Mg Basalt erupted from Back arc Basins and distinguished by its low Titanium Content and trace elements composition

A

Boninites

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16
Q

Tectonic Settings where Basalt Occurs

A

1)MORBs
2) OIBs
3) LIPs: Ocenic Plateaus and CFBs
4) Intra Continental Rifts
5) Subudction Related Basalts

17
Q

Type of Basalt in MORBs

A

Olivine Tholeiitic Basalt

18
Q

Distinctive of MORBs

A

Low K2O and Depleted of Incompatible Elements

19
Q

Subdivisions of MORBs

A

1) N-MORB - Extensive Partial Melting (20-30%)
deplete of Incompatible Elements
2) E-MORB - Small degree of Partial Melting of a depleted Mantle and enriched in Incomatible Elements

20
Q

Localized source of magma supply whose output thickens the basaltic crust and its immediate neighbourhood

A

Hotspots

21
Q

Basalts in OIBs are

A

Alkali

22
Q

Phases of OIBs

A

1) Development of Shied Volcano
2) Hiatus in which Erosion Occurs
3) Renewed Magmatism but this time more explosive and Alkali

23
Q

Basalts in LIPs are

A

Ol-Pl-phyric Low-K tholeiites

24
Q

Basalts in Intra continental Rifts are

A

Alkali (Nephelinnite and Mellilite)
Bimodal (Trachyte and Phonolite)

25
Q

Subduction Related Basalts

A

1) Low K Arc Tholeiites - High Al compared to MORB Tholeiite and occurs in young ocean island arcs
2) Medium K Arc Basalts - Mature Volcanic Island Arc
high alumina often Porphyritic w/ phenocrysts of Pl-Ol-Augite and Magnette
3) High K Arc Basalts - Relatively Scarce exceed by high K andesite (Shoshonites)

26
Q

Seismic Moho vs Petro Moho

A

Sesmic Moho occurs in between Layered Gabbro and Layered Ultramafic in between Layer 3 and Layer 4 while petrologic Moho coccurs in between Ultramafic cumulates and Residual Mantle Rocks

27
Q

Dominant rock in the Upper Mantle

A

Peridotites

28
Q

Fertile unaltered Mantle coposed of Oli+cpx+opx

A

Lherzolite

29
Q

Mostly Oli

A

Dunite

30
Q

Oli + Opx

A

Harzburgite

31
Q

Oli + Cpx

A

Wehrlite