Pressure-Temperature-Time Path of Granulites From the North PCMs - An Integrated Metamorphic Structural Geochronological Study

• Other Authors: HENSEN, BASTIAAN (hasPrincipalInvestigator), HENSEN, BASTIAAN (processor), THOST, DOUG E (processor), Australian Antarctic Data Centre (publisher)
• Format: Dataset
• Language: unknown
• Published: Australian Antarctic Data Centre
• Subjects: geoscientificInformation; MAJOR ELEMENTS; EARTH SCIENCE; SOLID EARTH; ROCKS/MINERALS/CRYSTALS; ELEMENTS; MINOR ELEMENTS; TRACE ELEMENTS; IGNEOUS ROCKS; METAMORPHIC ROCKS; geochemistry; prince charles mountains; proterozoic; XRF > X-Ray Fluorescence Spectrometer; Spectrometers; FIELD SURVEYS; LABORATORY; FIELD INVESTIGATION; Paleo Start Date; Paleo Stop Date; CONTINENT > ANTARCTICA > GEOGRAPHIC REGION > POLAR; East Antarctica; Prince Charles Mountains; Mac. Robertson Land; Porthos Range; Antarc*; Antarctica; Mac Robertson Land
• Online Access: https://researchdata.ands.org.au/pressure-temperature-time-geochronological-study/699631; https://data.aad.gov.au/metadata/records/ASAC_123; http://nla.gov.au/nla.party-617536

Metadata record for data from ASAC Project 123 Pressure-Temperature-Time Path of Granulites From the Northern Prince Charles Mountains - An Integrated Metamorphic Structural Geochronological Study See the link below for public details on this project. From the abstract of one of the referenced papers: The late Proterozoic basement of the Porthos Range northern Prince Charles Mountains, east Antarctica, is dominated by a suite of felsic to mafic granulites derived from igneous and, less importantly, sedimentary protoliths. Compositionally, they are broadly similar to granulites occurring along the Mac. Robertson Land coast and southern Prince Charles Mountains. Ultramafic to mafic orthypyroxene + clinopyroxene granulites with relict igneous layering occur as lenses within the felsic to mafic granulites, and show compositional evidence of a cumulate origin. The felsic to mafic granulites are intruded by several large charnockite bodies that have similarities to the Mawson Charnockite, and may have formed via a two-stage partial melting process. The charnockite and host granulites are chemically very similar, and both may have been derived from a common middle to lower crustal source region. Undepleted K/Rb ratios suggest retention of original chemistry, with variations being due to fractionation processes. Normalised trace element patterns resembling modern-day arc settings suggest that the Porthos Range granulites were possibly generated in a subduction zone environment.