Matuyama reversed chron

E675179

The Matuyama reversed chron is a long interval of predominantly reversed geomagnetic polarity that followed the Gauss–Matuyama reversal and lasted from about 2.58 to 0.78 million years ago.

All labels observed (2)

Label Occurrences
Matuyama reversed chron canonical 2
Matuyama chron 1

How this entity was disambiguated

Statements (30)

Predicate Object
instanceOf geomagnetic chron ⓘ
reversed polarity interval ⓘ
boundaryEvent Brunhes–Matuyama reversal ⓘ
chronCode C2r ⓘ
contains Jaramillo subchron ⓘ
Olduvai subchron ⓘ
duration about 1.8 million years ⓘ
endTime about 0.78 million years ago ⓘ
era Cenozoic ⓘ
evidenceFrom lava flow magnetization ⓘ
marine magnetic anomalies ⓘ
sedimentary rock remanent magnetization ⓘ
fieldType dipolar-dominated geomagnetic field ⓘ
follows Gauss–Matuyama reversal ⓘ
hasPolarity reversed ⓘ
includesAge Pleistocene ⓘ
lowerBoundaryDefinedBy Gauss–Matuyama reversal ⓘ
magneticFieldConfiguration south magnetic pole near geographic north ⓘ
namedAfter Motonori Matuyama ⓘ
partOf Cenozoic geomagnetic polarity timescale ⓘ
period Quaternary ⓘ
polarityRelativeToPresent opposite ⓘ
precededBy Gauss normal chron ⓘ
precedes Brunhes normal chron ⓘ
startTime about 2.58 million years ago ⓘ
upperBoundaryDefinedBy Brunhes–Matuyama reversal ⓘ
usedFor dating sedimentary sequences ⓘ
dating volcanic rocks ⓘ
geologic time correlation ⓘ
usedIn magnetostratigraphy ⓘ

How these facts were elicited

Referenced by (3)

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

Gauss normal chron → precedes → Matuyama reversed chron ⓘ
C2r → relatedTo → Matuyama chron ⓘ
linked to: Matuyama reversed chron