Zobrazeno 1 - 10
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pro vyhledávání: '"Claire E. Wade"'
Publikováno v:
Results in Geochemistry. 10:100020
Autor:
Claire E. Wade, Justin L. Payne, Karin M. Barovich, Anthony J. Reid, Elizabeth A. Jagodzinski, Stacey Curtis, Jesse Hill
Publikováno v:
Results in Geochemistry. 9:100019
Publikováno v:
Australian Journal of Earth Sciences. 67:31-58
Reconstructing ancient tectonic environments is inherently difficult and requires the integration of many datasets. Here we attempt to reconstruct the tectonic setting of a Proterozoic magm...
Autor:
Richard E. Ernst, Claire E. Wade, Chris Rogers, Michael A. Hamilton, Ulf Söderlund, Brian Cousens, S.S. Harlan, Sandra L. Kamo, Derek J. Thorkelson
Publikováno v:
Lithos. 2018. Vol. 314-315. P. 216-235
Three new U–Pb ID-TIMS isotopic ages confirm previous evidence for two geochemically distinct, early Mesoproterozoic pulses of mafic magmatism along the western margin of Laurentia. The first is a U–Pb baddeleyite age of 1590 ± 5 Ma from a dyke
Publikováno v:
Australian Journal of Earth Sciences. 65:447-463
The Mesoproterozoic Gawler Silicic Large Igneous Province (SLIP) in the Gawler Craton and Curnamona Province, southern Australia, comprises extensive felsic and lesser mafic volcanic sequences, with only limited sedimentary successions. The Roopena B
Autor:
Martin Hand, Justin L. Payne, Laura J. Morrissey, Claire E. Wade, Anthony Reid, Karin M. Barovich
Publikováno v:
Geological Society of America Abstracts with Programs.
Southern Australia, is host to a ca. 1590 Ma Silicic Large Igneous Province (SLIP) that produced approximately 100,000 km3 of felsic and mafic magmas within a 20 myr timeframe. Although a minor component, the mafic magmas within the SLIP present an o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fc69198774a47981e8215c1396ff0ffc
https://hdl.handle.net/11541.2/141371
https://hdl.handle.net/11541.2/141371
The ca 1600–1580 Ma time interval is recognised as a significant period of magmatism, deformation and mineralisation throughout eastern Proterozoic Australia. Within the northern Yorke Peninsula in South Australia, this period was associated with t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f39f16d721bda2704fdaaeae0f5a7e1f
https://hdl.handle.net/11541.2/132929
https://hdl.handle.net/11541.2/132929
The far northeastern Gawler Craton, South Australia, lies at the northern margin of one of the major building blocks of the Australian continent and is a region that is important in models for the Proterozoic tectonic evolution of Australia. However,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::edf12021e26dcdb39def37052a283bfa
https://hdl.handle.net/11541.2/130029
https://hdl.handle.net/11541.2/130029
Publikováno v:
Precambrian Research. :17-35
New ion microprobe (SHRIMP) U–Pb zircon data indicate that voluminous A-type volcanic rocks were extruded c. 1585 Ma in the Benagerie Ridge region of the north-central Curnamona Province in southern Australia. Incompatible trace element ratios and