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Mundts Complex

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Concordia diagrams of sample UM9 from the <b>Mundt’s</b> Concession <b>Complex</b> ( a ) ...
Published: 01 March 2021
Figure 4. Concordia diagrams of sample UM9 from the Mundt’s Concession Complex ( a ) and ( b ) and sample UM10 from the Sawmill Complex ( c ) and ( d ).
Journal Article
Published: 01 March 2021
South African Journal of Geology (2021) 124 (1): 7–16.
...Figure 4. Concordia diagrams of sample UM9 from the Mundt’s Concession Complex ( a ) and ( b ) and sample UM10 from the Sawmill Complex ( c ) and ( d ). ...
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Journal Article
Published: 01 June 2001
South African Journal of Geology (2001) 104 (2): 167–204.
...Carl R. Anhaeusser Abstract The southwestern portion of the Barberton greenstone belt is noteable for its varied and complex geology spanning at least 1360 Ma of earth history. A sequence dominated by metamorphosed Archaean komatiitic basalts and komatiites makes up most of the area occupied...
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Journal Article
Published: 01 December 2019
South African Journal of Geology (2019) 122 (4): 421–454.
...C.R. Anhaeusser Abstract Formations on the northwestern flank of the Barberton Greenstone Belt have hosted over 85% of all the gold recovered from the ca. 3550 to 3000 Ma Barberton Supergroup since early discoveries in 1872. This sector of the greenstone belt also happens to coincide with a complex...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1968
AAPG Bulletin (1968) 52 (5): 767–781.
... and is reflected in the stratigraphic record by clastic wedges, unconformities, and structural complexities. Outside of the area adjacent to the Antler belt, Meramecian instability is reflected by the initiation of strongly subsiding basins in Utah and Idaho, and by an epeirogenically produced regional sub...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1956
AAPG Bulletin (1956) 40 (4): 789.
...Phil A. Mundt ABSTRACT In central Montana the accumulation of oil in the so-called “Heath” and “Amsden” formations is controlled by complex stratigraphic relationships. These relationships, however, are clarified by an analysis of the effect of tectonic elements upon depositional patterns...
Image
Google Earth image of the eastern sector of the Jamestown Schist Belt showi...
Published: 01 December 2019
Figure 11. Google Earth image of the eastern sector of the Jamestown Schist Belt showing the location of the New Consort GM (top right) and the Mundt’s Concession (top centre - MC ) and Handsup (lower centre - H ) layered ultramafic complexes. The Mundt’s Concession Complex forms a large
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1984
AAPG Bulletin (1984) 68 (2): 178–195.
... of Mississippian strata. The Lower Pennsylvanian shoreline finally extended onto the cratonic interior in eastern North Dakota. Initial Tyler sediments were deposited as a deltaic and fluviolacustrine complex succeeded by littoral deposits as the Early Pennsylvanian shoreline transgressed eastward across the shelf...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1965
AAPG Bulletin (1965) 49 (11): 1824–1832.
...E. EARL NORWOOD ABSTRACT Central Montana has had a complex structural and sedimentary history, especially in the area of the present-day Central Montana uplift. Precambrian and Cambrian subsidence was accompanied by the deposition of more than 13,000 feet of clastics in an east-west-trending trough...
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Journal Article
Published: 01 March 2017
South African Journal of Geology (2017) 120 (1): 101–132.
..., with the result that the stronger mineralising systems tend to be concentrated in finite gold “camps” which host the larger deposits and numerous styles of mineralisation, e.g., the Sheba-Fairview Complex on the refolded arcuate Eureka and Ulundi synclines. Gold hosted in BIFs is a widespread association...
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Journal Article
Published: 01 March 2021
South African Journal of Geology (2021) 124 (1): 1–4.
... that the rocks mapped by Carl in the Jamestown schist belt, as well as those mapped by Morris and Carl along the northern flank of the BML earlier, were altered komatiites. They included the presence of layered komatiitic complexes which Carl named the Mundt’s Concession and Handsup bodies in the eastern part...
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Series: GSA Special Papers
Published: 15 October 2019
DOI: 10.1130/2019.2543(03)
EISBN: 9780813795430
... varying in steepness, deeply incised valleys, flat terraces, and moist floodplains, etc. provides a complex system. The vegetation on each of these different landscape types immediately prior to settlement and the absence of fossiliferous sites on each illustrates the difficulty in providing a generalized...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1994
AAPG Bulletin (1994) 78 (4): 519–543.
..., and foreland platforms ( Fulthorpe and Schlanger, 1989 ). During deposition, the prevailing climate was relatively warm and humid, characteristic of open oceanic tropical–subtropical settings ( Fulthorpe and Schlanger, 1989 ). In contrast, the Miocene history of the Tethyan region reflects complex...
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Journal Article
Published: 27 August 2019
Journal of Sedimentary Research (2019) 89 (8): 761–783.
... surfaces. Controversy concerning the contact of the Heath Formation and the overlying Tyler Formation, as well as the stratigraphic position of the Bear Gulch Limestone, has existed throughout the history of stratigraphic research in central Montana. The majority of workers ( Mundt 1956 ; Norton 1956...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1987
AAPG Bulletin (1987) 71 (3): 281–297.
... they are significant in petroleum exploration, these structures have been the subject of numerous seismic studies (McClintock, 1976; Burbury, 1977 ; Kenyon, 1977 ; Chevron Standard Limited, 1979; Hriskevich et al, 1980 ; Baria et al, 1982 ; Mundt, 1982 ; Bally, 1983 ; Frost et al, 1983 ). Bubb and Hatlelid...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 2001
AAPG Bulletin (2001) 85 (1): 131–148.
... in the development and distribution of reservoir facies. The Central Montana platform has undergone a complex tectonic history exhibiting episodic reversal of movement along bounding and internal faults (e.g., see Staggs, 1956 ; Sonnenberg, 1956 ; Alpha, 1958 ; Norwood, 1965 ; Shepard, 1993 ). The Custer...
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Journal Article
Journal: PALAIOS
Published: 15 August 2019
PALAIOS (2019) 34 (8): 383–392.
... R freeware (R v. 3.4.1) ( R Core Development Team 2016 ) using the following packages: dplyr ( Wickham et al. 2019 ), tidyr ( Wickham and Henry 2017 ), binom ( Doraj-Raj 2014 ), factoextra ( Kassambara and Mundt 2017 ), ggplot2 ( Wickham 2009 ), ggExtra ( Attali 2017 ), ggridges ( Wilke 2017...
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Journal Article
Journal: Geosphere
Published: 01 April 2013
Geosphere (2013) 9 (2): 367–377.
... the scanning. The experiment ( Fig. 1 ) was designed to reduce the complexity of the surface and targets and allows for the effects of different scan settings and geometries to be isolated and evaluated. The cups (0.090 m diameter, 0.132 m height) were filled with sand to ensure that their position...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1956
AAPG Bulletin (1956) 40 (8): 1915–1934.
...Philip A. Mundt ABSTRACT In central Montana the so-called “Amsden” formation consists of three lithologic divisions—an upper dolomite unit, a middle brownish limestone unit, and a lower sequence of red shale and sandstone beds. The dolomite unit is lithologically, stratigraphically...
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Journal Article
Published: 01 January 2006
Journal of Sedimentary Research (2006) 76 (1): 91–116.
... quality ( Epting 1980 , 1989 ; McArthur and Helm 1982 ; Wright and Hardian 1982 ; Mundt 1983 ; May and Eyles 1985 ; Grange and Davies 1985 ; Leamon and Parsons 1986 ; Longman et al. 1987 ; Mayall and Cox 1988 ; Dolan and Hermany 1988 ; Rudolph and Lehmann 1989 ; Gibson-Robinson et al. 1990...
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