The Vicuña Mackenna Batholith (Spanish: Batolito Vicuña Mackenna) is a group of plutons in the Chilean Coast Range of northern Chile. The plutons of the batholith formed (cooled from magma to rock) between the Early Jurassic and the Late Cretaceous (192–98 Ma). The magmas that formed the batholith originated in Earth's mantle and have not suffered any significant . A group of Early Cretaceous plutons were intruded syn-tectonically on the Atacama Fault.
Attributes | Values |
---|---|
rdf:type | |
rdfs:label |
|
rdfs:comment |
|
name |
|
geo:lat |
|
geo:long |
|
dcterms:subject | |
Wikipage page ID |
|
Wikipage revision ID |
|
Link from a Wikipage to another Wikipage |
|
sameAs | |
dbp:wikiPageUsesTemplate | |
age |
|
country | |
period |
|
region | |
type | |
georss:point |
|
has abstract |
|
namedfor | |
prilithology |
|
prov:wasDerivedFrom | |
page length (characters) of wiki page |
|
foaf:isPrimaryTopicOf | |
geo:geometry |
|
is Link from a Wikipage to another Wikipage of | |
is foaf:primaryTopic of |