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The Hohonu Batholith of North Westland, New Zealand: Granitoid compositions controlled by source H
2
O contents and generated during tectonic transition
Tod E. Waight
*
, Stephen D. Weaver, Roderick J. Muir, Roland Maas, G. Nelson Eby
*
Corresponding author af dette arbejde
Geologi
72
Citationer (Scopus)
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2
O contents and generated during tectonic transition'. Sammen danner de et unikt fingeraftryk.
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Alfabetisk
Fysik og astronomi
batholiths
100%
tectonics
71%
New Zealand
67%
plagioclase
57%
amphiboles
31%
melting
28%
garnets
19%
lithosphere
14%
magma
13%
coasts
12%
dehydration
11%
silicon dioxide
6%
collisions
5%
interactions
3%
Geo- og miljøvidenskab
batholith
50%
granitoid
44%
plagioclase
41%
tectonics
29%
transition
28%
melting
25%
amphibole
23%
garnet
20%
Cretaceous
16%
dehydration melting
15%
crustal thinning
15%
complex formation
14%
crustal thickening
13%
metasediment
13%
Ordovician
10%
lithosphere
10%
isotopic composition
9%
collision
9%
silica
9%
magma
8%
melt
8%
coast
6%
Kemiske forbindelser
Melting
39%
Thickening
14%
Collision
11%
Dehydration
9%