Crust-Enriched, Mantle-Derived Tonalites in the Early Proterozoic Penokean Orogen of Wisconsin
- 1 March 1987
- journal article
- Published by University of Chicago Press in The Journal of Geology
- Vol. 95 (2) , 139-154
- https://doi.org/10.1086/629116
Abstract
No abstract availableThis publication has 31 references indexed in Scilit:
- Island arc and continent-building magmatism — A review of petrogenic models based on experimental petrology and geochemistryPublished by Elsevier ,2003
- An evaluation of the behavior of the rare earth elements during the weathering of sea-floor basaltPublished by Elsevier ,2002
- Rapid production of continental crust 1.7 to 1.9 b.y. ago: Nd isotopic evidence from the basement of the North American mid-continentGSA Bulletin, 1985
- Trace element and isotopic effects of combined wallrock assimilation and fractional crystallizationEarth and Planetary Science Letters, 1981
- Mineral equilibria and crystallization conditions in the late Precambrian Wolf River rapakivi massif, WisconsinAmerican Journal of Science, 1980
- The role of sphene as an accessory phase in the high-pressure partial melting of hydrous mafic compositionsEarth and Planetary Science Letters, 1979
- A variably veined suboceanic upper mantle—Genetic significance for mid-ocean ridge basalts from geochemical evidenceGeology, 1979
- Gneiss and migmatite of Archean age in the Precambrian basement of central WisconsinGeology, 1977
- Geology and Rb-Sr Chronology of Middle Precambrian Rocks in Eastern and Central WisconsinGSA Bulletin, 1975
- The petrological evolution of island arc systemsJournal of the Geological Society, 1974