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Ivanhoe Member

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Journal Article
Published: 01 March 1980
Journal of Sedimentary Research (1980) 50 (1): 91–116.
... of Lower Paleozoic platform margin. The upward-shallowing platform sequence consists of shallow subtidal ribbon-laminated carbonates (Patterson Member) overlain by shoal water to tidal flat massive dolomites and fenestral cryptalgal carbonates (Austinville and Ivanhoe Members) that pass up into red...
Journal Article
Published: 01 July 1994
Canadian Journal of Earth Sciences (1994) 31 (7): 1182–1196.
... of the KSZ, dykes exhibiting clouded feldspar and high-alumina amphiboles occur on the upthrown side of the Budd Lake fault zone, which has a trend similar to that of the Ivanhoe Lake fault. Therefore a second thrust block may exist, raising the possibility that the KSZ represents the basal member...
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1966
AAPG Bulletin (1966) 50 (10): 2245–2259.
... in the Lower member of the Tyler Formation. Reconstruction of the pre-Amsden structure and the Tyler-Heath paleogeology shows that oil accumulations at Sumatra, Stensvad, Ivanhoe, Keg Coulee, Bascom, Melstone, and Big Wall fields occur where the paleostructural position of the lower Tyler sandstone beds...
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—Southwest-northeast paleostructural cross section A-A′ through Keg Coulee, Ivanhoe, and Stensvad fields showing relation of producing sandstone beds to subcrop of Limestone member of Heath Formation. Location of section A-A′ is shown on Figures 4 and 5.
Published: 01 October 1966
FIG. 6. —Southwest-northeast paleostructural cross section A-A′ through Keg Coulee, Ivanhoe, and Stensvad fields showing relation of producing sandstone beds to subcrop of Limestone member of Heath Formation. Location of section A-A′ is shown on Figures 4 and 5 .
Book Chapter

Author(s)
Graham Tegerdine
Series: Geological Society, London, Memoirs
Published: 30 October 2020
DOI: 10.1144/M52-2018-3
EISBN: 9781786205070
.... Planned export of produced fluids was via an 8 inch, 6 km-long, pipeline to the Renee manifold and then onwards through a 21 km-long pipeline to the Amerada Hess-operated AH001 FPF in the nearby Ivanhoe–Rob Roy fields to the north ( Fig. 6 ). The Cromarty Sandstone Member was excluded from the development...
Journal Article
Published: 01 July 1994
Canadian Journal of Earth Sciences (1994) 31 (7): 1134–1145.
...Urs K. Mäder; John A. Percival; Robert G. Berman Abstract Amphibole mixing properties and standard state properties for the end members tremolite, tschermakite, pargasite, ferrotremolite, ferrotschermakite, and ferropargasite have been refined through analysis of relevant phase equilibrium...
Image
(a) Map of the North Sea rift system showing the position of the Rattray Volcanic Province at the triple junction of the Viking Graben, Central Graben and Outer Moray Firth Basin. Adapted from Fraser et al. 2002. (b) Present day thickness and structure map of the Rattray Volcanics Member constructed using well and seismic mapping data. Structures adapted from Fraser et al. 2002. Volcanic centres of Smith &amp; Ritchie (1993): F, Fisher Bank Volcanic Centre; G, Glenn Volcanic Centre; I, Ivanhoe Volcanic Centre.
Published: 10 January 2019
Member constructed using well and seismic mapping data. Structures adapted from Fraser et al. 2002 . Volcanic centres of Smith & Ritchie (1993) : F, Fisher Bank Volcanic Centre; G, Glenn Volcanic Centre; I, Ivanhoe Volcanic Centre.
Journal Article
Journal: Economic Geology
Published: 01 August 2019
Economic Geology (2019) 114 (5): 1013–1014.
... and is at points chronologically out of order, leading to some confusion about the timing of key events. For example, it remains unclear the timing of Ivanhoe Mines key discovery holes OTD140, OTD150, and OTD159 in relation to BHP’s decision to not claw back part ownership of Oyu Tolgoi. These drill holes...
Series: Geological Society, London, Memoirs
Published: 01 January 2003
DOI: 10.1144/GSL.MEM.2003.020.01.36
EISBN: 9781862393950
... Abstract The Ivanhoe, Rob Roy and Hamish Fields lie in the Moray Firth of the UKCS in Block 15/21 and contain undersaturated oil trapped in the prolific Upper Jurassic Piper reservoir in tilted fault block traps. The fields were brought on stream in 1989 and since then the reservoir model has...
Journal Article
Journal: Economic Geology
Published: 01 December 2004
Economic Geology (2004) 99 (8): 1665–1686.
... ). The aerially restricted distribution of the middle member (Tep 2), as well as more abundant ash-flow and lapilli tuffs at Midas compared to the Ivanhoe area, suggests localized basin formation at Midas during this time and closer proximity to a source. The ages of the fine-grained white tuff (Tepu...
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Journal Article
Journal: SEG Discovery
Published: 01 April 2021
SEG Discovery (2021) (125): 19–26.
... of the Southern Korean peninsula is prospective for epithermal precious metal deposits, spatially associated with basin-scale brittle fault systems in Cretaceous volcanic terranes. South Korea is an underexplored jurisdiction, with limited modern exploration and drilling until the mid-1990s, when Ivanhoe Mines...
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First thumbnail for: Epithermal Precious Metal Deposits in South Korea—...
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Journal Article
Journal: Economic Geology
Published: 01 September 2021
Economic Geology (2021) 116 (6): 1483–1484.
..., on page 25 in the Introduction to Copper Deposits, the authors state that Oyu Tolgoi was discovered “in 2001 by Canadian-based Ivanhoe Mines…,” which is a false statement. The original discovery was made by BHP in the fall of 1996. After mapping and conducting geophysical and geochemical surveys at Oyu...
Journal Article
Published: 10 January 2019
Journal of the Geological Society (2019) 176 (3): 462–481.
... Member constructed using well and seismic mapping data. Structures adapted from Fraser et al. 2002 . Volcanic centres of Smith & Ritchie (1993) : F, Fisher Bank Volcanic Centre; G, Glenn Volcanic Centre; I, Ivanhoe Volcanic Centre. ...
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Image
Regional map showing the distribution of mid-Miocene (ca. 17–15 Ma) volcanism in the Pacific Northwest (after Benson and Mahood, 2016). Extents of Columbia River Flood Basalt (CRB) Group members are split into Steens Basalt and younger members (Imnaha, Grande Ronde, Picture Gorge, Wanapum, Saddle Mountain) based on Reidel et al. (2013a), and generalized locations of feeder dikes are after Tolan et al. (1989), Camp et al. (2013), and Reidel et al. (2013b). Caldera locations are from this study, Rytuba and McKee (1984), Rytuba and Vander Meulen (1991), Benson and Mahood (2016), Coble and Mahood (2016), and Henry et al. (2016), and are labeled with the following symbols: V—Virgin Valley caldera, B—Badger Mountain caldera, H—Hanging Rock caldera, CC—Cottonwood Creek caldera, M—McDermitt caldera, R—Rooster Comb caldera, CR—proposed caldera at Castle Rock. Contemporaneous lava centers are shown as yellow dots and are labeled with the following symbols: SC—Silver City, LJ—Little Juniper Mountain, HH—Horsehead Mountain, JB—Jackass Butte, SW—Swamp Creek Rhyolite, TM—Twenty Mile Creek Rhyolite, BB—Bald Butte, D—Drum Hill, HV—Hawks Valley–Lone Mountain, S—Sleeper Rhyolite, SR—Santa Rosa–Calico, I—Ivanhoe, J—Jarbidge. Other symbols: Y—Yellowstone caldera, JdF—Juan de Fuca plate, NNR—northern Nevada Rift. Isopleths of 0.704 and 0.706 87Sr/86Sri are after Benson and Mahood (2016, and references therein).
Published: 23 June 2017
Figure 1. Regional map showing the distribution of mid-Miocene (ca. 17–15 Ma) volcanism in the Pacific Northwest (after Benson and Mahood, 2016 ). Extents of Columbia River Flood Basalt (CRB) Group members are split into Steens Basalt and younger members (Imnaha, Grande Ronde, Picture Gorge
Image
(a) Magnetic anomaly map of the Rattray area highlighting the magnetic anomaly coincident with the Buchan–Glenn Horst structure. Volcanic centres of Smith &amp; Ritchie (1993): F, Fisher Bank Volcanic Centre; G, Glenn Volcanic Centre; I, Ivanhoe Volcanic Centre. Reproduced from the British Geological Survey Map data at the original scale of 1:50 000. Licence 2016/103 ED British Geological Survey. ©UKRI. All rights reserved. Positions of seismic lines shown in Figures 6, 7 and 9 are highlighted on the inset map. (b) Seismic line A–A′ west–east across the Buchan–Glenn Horst over the peak of the magnetic anomaly and (c) interpretation. The Rattray Volcanics Member is c. 1.2 km thick across this section of the Buchan–Glenn Horst. It lies above a thin Permian carbonate succession above the Devonian–Carboniferous Old Red Sandstone Group with laterally continuous seismic reflections. There is no obvious large-scale volcanic vent structure observed in the Rattray succession, nor kilometre-scale discordant seismic reflections in the sub-Rattray stratigraphy, which would indicate an intrusive sill complex feeding a large central volcano. A sill cross-cuts the volcanic reflections in the Rattray package, indicative of later-stage intrusion that did not feed the majority of the Rattray volcanism. Inclined seismic reflections in the Rattray sequence downlap the substrate, probably a hyaloclastite delta.
Published: 10 January 2019
Fig. 6. ( a ) Magnetic anomaly map of the Rattray area highlighting the magnetic anomaly coincident with the Buchan–Glenn Horst structure. Volcanic centres of Smith & Ritchie (1993) : F, Fisher Bank Volcanic Centre; G, Glenn Volcanic Centre; I, Ivanhoe Volcanic Centre. Reproduced from
Journal Article
Journal: Geosphere
Published: 01 February 2008
Geosphere (2008) 4 (1): 36–74.
... middle Miocene basins studied—Chimney, Ivanhoe, Carlin, and Elko, from west to east—was an upland that underwent prolonged middle Tertiary exposure and moderate erosion. All four basins began to retain sediments at ca. 16 Ma. Eruption of volcanic flows in the Chimney and Ivanhoe basins produced short...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 2018
AAPG Bulletin (2018) 102 (7): 1213–1237.
... of the set, so it is also known as the “80/20 rule” ( Crovelli, 1995 ; Aguilera and Ripple, 2011 ). By ranking the reservoir sizes with a high degree of exploration according to area, larger field sizes were found to correspond to greater impact on the total resources ( Ivanhoe, 1976 ). In the mid-twentieth...
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First thumbnail for: Petroleum resources in the Nanpu sag, Bohai Bay Ba...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1965
AAPG Bulletin (1965) 49 (11): 1824–1832.
... into the sea in this vicinity and that the sediment was widely distributed in a shallow-water nearshore environment. The lower member of the Tyler is productive at Big Wall, Melstone, Keg Coulee, Ivanhoe Dome, Stensvad, and Sumatra fields ( Fig. 13 ). Sumatra is by far the largest with about 50 million...
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Journal Article
Journal: Geosphere
Published: 01 October 2010
Geosphere (2010) 6 (5): 691–730.
... ; John, 2001 ; John et al., 2003 ; Wallace, 2003 ). Great Basin bimodal igneous rocks are broadly characterized by basaltic and rhyolitic end-member compositions. Ages and compositions of the bimodal suite, however, vary in age and composition across the Great Basin Province. They include ages...
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First thumbnail for: Development of an igneous rock database with geolo...
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Journal Article
Journal: SEG Discovery
Published: 01 October 2005
SEG Discovery (2005) (63): 1–52.
... Economic Geology ARCHIVE Funded by the Society of Economic Geologists On DVD ~ Linked, Canada Foundation and generously supported by Charles Fipke, searchable index ~ Stewart Blusson, and Ivanhoe Mines Ltd. Linked references ~ Available this year ~ Members will be noti ed of availability by e...