Geology of Grand Canyon, Northern Arizona (With Colorado River Guides): Lee Ferry to Pierce Ferry, Arizona 1989
DOI: 10.1029/ft115p0117
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Potential petroleum source rocks in the Late Proterozoic Chuar Group, Grand Canyon, Arizona

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Cited by 10 publications
(9 citation statements)
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“…Figure 1 depicts a map of the regional extent and outcrop locations of the Chuar rocks. Exposures in the Grand Canyon reach a thickness of approximately 5,370 ft, and the rocks consist of organic-rich gray-black shale and siltstone interbedded with sandstones and cryptalgal and stromatolitic carbonates (Reynolds et al, 1988;Palacas, 1992). The Chuar Group contains the lower Galeros Formation and the overlying Kwagunt Formation (Figure 2).…”
Section: Geologic Settingmentioning
confidence: 99%
See 1 more Smart Citation
“…Figure 1 depicts a map of the regional extent and outcrop locations of the Chuar rocks. Exposures in the Grand Canyon reach a thickness of approximately 5,370 ft, and the rocks consist of organic-rich gray-black shale and siltstone interbedded with sandstones and cryptalgal and stromatolitic carbonates (Reynolds et al, 1988;Palacas, 1992). The Chuar Group contains the lower Galeros Formation and the overlying Kwagunt Formation (Figure 2).…”
Section: Geologic Settingmentioning
confidence: 99%
“…The lithologies indicate various cyclical depositional environments, including a sediment-starved basin rich in organic material, coastal and alluvial plains, paludal swamp, and nearshore aqueous. Deposition of the Chuar Group occurred on a marine embayment on the passive edge of a continent (Reynolds et al, 1988).…”
Section: Geologic Settingmentioning
confidence: 99%
“…Figure 17 depicts a map of the regional extent and outcrop locations of the Chuar rocks. Exposures in the Grand Canyon reach a thickness of approximately 5,370 ft, and the rocks consist of organic-rich gray-black shale and siltstone interbedded with sandstones and cryptalgal and stromatolitic carbonates (Reynolds et al, 1988;Palacas, 1992). The Chuar Group contains the Galeros Formation and the overlying Kwagunt Formation (Figure 18).…”
Section: Chuar Group (Precambrian Paradox Basin) Geologic Settingmentioning
confidence: 99%
“…The lithologies indicate various cyclical depositional environments, including a sediment-starved basin rich in organic material, coastal and alluvial plains, paludal swamp, and nearshore marine. Deposition of the Chuar Group occurred on a marine embayment on the passive edge of a continent (Reynolds et al, 1988).…”
Section: Chuar Group (Precambrian Paradox Basin) Geologic Settingmentioning
confidence: 99%
“…New studies and sampling, conducted in the late 1980s-early 1990s, led by Reynolds and/or l?alacas, along with Elston and other assoaates (Re~olds and Elston 1986;Reynolds, I?alacas and Elston 1988;Reynolds, Palacas and Elston 1989;Palacas and Reynolds 1989;Chidsey, Allison, and Palacas 1990;Palacas 1992;Pawlewicz and Palacas1992;' Palacas 1993;Lillis, Palacas, and Warden 1995) have demonstrated that the Chuar includes potential hydrocarbon source beds in both Arizona and Utah, finally attracting the attention of the petroleum industry.…”
Section: Sourcesmentioning
confidence: 99%