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Geol 2312 Igneous and Metamorphic Petrology. Lecture 19 Anorthosites and the Anorthosite Problem. March 11, 2009. Global Occurrences of Anorthosite. 1. Archean anorthosite 2. Proterozoic “massif-type” anorthosite plutons 3. Centimeter-to-100m thick layers in layered mafic intrusions
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Geol 2312 Igneous and Metamorphic Petrology Lecture 19 Anorthosites and the Anorthosite Problem March 11, 2009
Global Occurrences of Anorthosite • 1. Archean anorthosite • 2. Proterozoic “massif-type” anorthosite plutons • 3. Centimeter-to-100m thick layers in layered mafic intrusions • 4. Thin cumulate layers in ophiolites/oceanic crust • 5. Small inclusions in other rock types (xenoliths and cognate inclusions) • 6. Lunar highland anorthosites (after Ashwal, 1993) Streikeisen (1991)
Archean Anorthosites • Hi-Ca plagioclase (An >80) • Equant crystal habit • Pl megacrysts in a gabbroic • matrix • Sill-like bodies • Associated with gabbroic • intrusions in greenstone • belts • Commonly metamorphosed • and deformed
Massif-type Anorthosites • Proterozoic age (1.7-0.9 Ga) • Intermediate Pl composition (An 65-40) • Tabular crystal habit • Pl-adcumulates common (minor interstitial mafics) • Large pluton-scale bodies • Anorogenic setting • Associated with K-/Fe-rich gabbros (jonuites) and “dry” felsic rocks (charnokites) Grenville Province
Anorthosite Layers/Inclusions in Mafic Layered Intrusions Bushveld Complex Skaergaard Intrusion Stillwater Complex
Anorthositic Rocks of the Duluth Complex and Related Rocks of NE MN Anorthositic Rock–bearing Units
Anorthosite Inclusions of the Beaver Bay Complex • 90-100% Plagioclase • An 70-90 • Mafic phases – Ol, Opx • Single grains to 500m block • Isotopes indicate older crustal component • Enclosing diabase NOT chilled against inclusions
Lake Superior AnorthositesA 150 Year Puzzle Norwood (1852) Lawson (1893) Winchell (1899)
Beaver River DiabaseHost of Anorthosite Inclusions Leveaux Porphyry Lutsen Tofte Silver Bay Carlton Peak Split Rock
Porphyritic Fe-Diorite SillsLeveaux Porphyry & Cabin Creek Porphyritic Diorite
troctolitic anorthosite Anorthositic Series of the Duluth Complex poikilitic olivine anorthosite olivine leucogabbro gabbroic anorthosite olivine-oxide leucogabbro
“An Igneous Breccia” R. Taylor, 1964 pOGA (PPocf) TA (PpO) An (mPP) mTA (mPpO) GA (cPpcf) TA (cPPOc)
Summary of Lithologic and Structural Relationships of Anorthositic Series rocks in the Snowbank Lake Quadrangle
Fo-An Relationships
Plagioclase Zonation Patterns Complex Patterns Outer jump in An – Decompression? Hi-P Lo-P
Weiblen and Morey (1980) Model for the formation of the Anorthositic and Layered (Troctolitic) Series
Major Problem: No Evidence for Significant Upper Crustal Ultramafic Rocks
AS Parent Magma = Plagioclase Crystal Mush
Geochronology of MCR IntrusionsAnorthositic Series ≈ Layered Series