Publication Date:
2021-03-29
Description:
The Chilean accretionary wedge is part
of a Late Paleozoic subduction complex
that developed during subduction of the
Pacific plate underneath South America.
The wedge is commonly subdivided
into a structurally lower Western Series
and an upper Eastern Series. Understanding
the contact between both series
has been a long standing problem
and is fundamental for the understanding
of the evolution of the wedge system.
We show the progressive development
of structures and finite strain from
the least-deformed rocks in the eastern
part of the Eastern Series of the accretionary
wedge to higher grade schist of
the Western Series at the Pacific coast...
Description:
conference
Keywords:
551
;
VEX 500
;
VAE 812
;
VAE 500
;
Chile {Geologie}
;
Variszisch-herzynische Orogene {Geologie}
;
Geotektonische Entwicklung der Erdkruste {Geologie}
;
Chile
;
Jungpaläozoikum
;
Akkretionskeil
Language:
German
Type:
anthologyArticle
,
publishedVersion
Format:
application/pdf
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