Geological characteristics and tectonic setting of proterozoic iron oxide (Cu U Au REE) deposits

MW Hitzman, N Oreskes, MT Einaudi - Precambrian research, 1992 - Elsevier
Recent work on the Olympic Dam Cu U Au Ag deposit, South Australia, the Wernecke
Mountain breccias, Yukon, the Kiruna iron ore district, Sweden, and the southeast Missouri …

The roots of ash flow calderas in western North America: windows into the tops of granitic batholiths

PW Lipman - Journal of Geophysical Research: Solid Earth, 1984 - Wiley Online Library
Large‐volume ash flow eruptions and associated caldera collapses provide a direct link with
subvolcanic granitic plutons of batholithic dimensions. The eruptive history, structural …

A Paleoproterozoic Andean-type iron oxide copper-gold environment, the Great Bear magmatic zone, Northwest Canada

L Ootes, D Snyder, WJ Davis, P Acosta-Góngora… - Ore Geology …, 2017 - Elsevier
Iron oxide copper-gold (IOCG) and associated iron-oxide apatite (IOA) styles of metallic
mineralization are recognized throughout the Paleoproterozoic Great Bear magmatic zone …

Kiruna-type deposits; their origin and relationship to intermediate subvolcanic plutons in the Great Bear magmatic zone, Northwest Canada

RS Hildebrand - Economic Geology, 1986 - pubs.geoscienceworld.org
Magnetite-apatite-actinolite rocks, similar to those at Kiruna, Sweden, and the St. Francois
Mountains, Missouri, are associated with seven epizonal plutons that intrude andesitic …

Arc–continent collision in the Ordovician of western Ireland: stratigraphic, structural and metamorphic evolution

D Brown, PD Ryan, PD Ryan, JF Dewey - Arc-continent collision, 2011 - Springer
The geology of western Ireland preserves a record of the collision of the Lough Nafooey arc
with the Laurentian margin which caused the mid-Ordovician Grampian Orogeny …

Short-lived 1.9 Ga continental margin and its destruction, Wopmay orogen, northwest Canada

PF Hoffman, SA Bowring - Geology, 1984 - pubs.geoscienceworld.org
A 1.9 Ga continental margin in the northwest of the Canadian Shield evolved in less than 15
my from a zone of crustal stretching, through a phase of passive-margin subsidence, to …

[CARTE][B] Did westward subduction cause Cretaceous-Tertiary orogeny in the North American Cordillera?

RS Hildebrand - 2009 - books.google.com
Within the Sonora segment to the south, break-off magmatism was also prevalent. Both the
Canadian and Sonoran segments have abundant porphyry copper mineralization …

Tectono-magmatic evolution of the 1.9-Ga Great Bear magmatic zone, Wopmay orogen, northwestern Canada

RS Hildebrand, PF Hoffman, SA Bowring - Journal of Volcanology and …, 1987 - Elsevier
Abstract The 1875-1840-Ma Great Bear magmatic zone is a 100-km wide by at least 900-km-
long belt of predominantly subgreenschist facies volcanic and plutonic rocks that …

Arc and slab-failure magmatism in Cordilleran batholiths II–The Cretaceous Peninsular Ranges batholith of southern and Baja California

RS Hildebrand, JB Whalen - Geoscience Canada, 2014 - erudit.org
Ever since the late 1960s when Warren Hamilton proposed that the great Cordilleran
batholiths of the western Americas are the roots of volcanic arcs like the Andes and were …

The Calderian orogeny in Wopmay orogen (1.9 Ga), northwestern Canadian shield

RS Hildebrand, PF Hoffman, SA Bowring - Bulletin, 2010 - pubs.geoscienceworld.org
The Wopmay orogen is a Paleoproterozoic orogenic belt formed in part by the accretion of
Hottah terrane, an east-facing continental magmatic arc, to the western margin of the …