From Wikipedia, the free encyclopedia
Tierra del Fuego Igneous and Metamorphic Complex
is a geological
basement complex
known from
boreholes
in northern
Tierra del Fuego
.
[1]
[2]
The complex is made up of
foliated
igneous rocks of
Cambrian
age including
orthogneiss
.
[1]
[2]
It underlies
unconformably
the
Jurassic
Tobifera Formation
. The
protoliths
of
Cordillera Darwin Metamorphic Complex
are unrelated to Tierra del Fuego Igneous and Metamorphic Complex despite present-day proximity.
[1]
References
[
edit
]
- ^
a
b
c
Herve, F.
; Fanning, C.M.;
Pankhurst, R.J.
;
Mpodozis, C.
; Klepeis, K.; Calderon, M.; Thomson, S.N. (2010).
"Detrital zircon SHRIMP U?Pb age study of the Cordillera Darwin Metamorphic Complex of Tierra del Fuego: sedimentary sources and implications for the evolution of the Pacific margin of Gondwana"
(PDF)
.
Journal of the Geological Society, London
.
167
(3): 555?568.
doi
:
10.1144/0016-76492009-124
.
S2CID
129413187
.
- ^
a
b
Herve, F.
; Faundez, V.; Calderon, M.; Massonne, H.-J.; Willner, A.P. (2007). "Metamorphic and plutonic basement complexes". In Moreno, Teresa; Gibbons, Wes (eds.).
The Geology of Chile
.
Geological Society of London
. pp. 7?20.
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Terranes
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Sedimentary
formations
and groups
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Batholiths
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Metamorphic
complexes
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Faults
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