Ferrar Dolerite

E653121

Ferrar Dolerite is a widespread Jurassic-age igneous rock formation in Antarctica, notable for forming prominent sills and cliffs within the Transantarctic Mountains.

All labels observed (1)

Label Occurrences
Ferrar Dolerite canonical 2

How this entity was disambiguated

Statements (45)

Predicate Object
instanceOf dolerite
igneous rock formation
mafic intrusive rock
ageRange Early Jurassic
approximateAgeMa 183
associatedWith Jurassic magmatism in Antarctica
breakup of Gondwana
composition Fe-Ti oxides
clinopyroxene
orthopyroxene
plagioclase feldspar
country Antarctica
discoveredBy early Antarctic explorers and geologists in the Transantarctic Mountains
distribution widespread along Transantarctic Mountains
emplacementStyle dike swarm
sill complex
exposedIn Transantarctic Mountains
forms cliffs
dikes
sills
geologicAge Jurassic
hostRocks Beacon Supergroup
lithology dolerite
locatedIn Antarctica
magmaticAffinity tholeiitic basaltic
namedAfter Ferrar Glacier region
linked to: Ferrar Glacier
notableExposure McMurdo Dry Valleys
Queen Alexandra Range
Victoria Land
overlies Beacon Supergroup sedimentary rocks
partOf Ferrar Large Igneous Province
relatedTo Karoo-Ferrar Large Igneous Province
researchField Antarctic geology
igneous petrology
large igneous provinces
significance important for reconstructing Gondwana breakup
important for studying Jurassic magmatism
key marker horizon in Transantarctic stratigraphy
tectonicSetting continental flood basalt province
texture medium-grained
subophitic
thickness locally hundreds of meters
underlies Jurassic volcanic rocks in some areas
weatheringExpression prominent escarpments
steep cliffs

How these facts were elicited

Referenced by (2)

Full triples — surface form annotated when it differs from this entity's canonical label.

Transantarctic Mountains contains Ferrar Dolerite
Beacon Supergroup underlies Ferrar Dolerite