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![Schematic chronostratigraphic chart to show the spatial and temporal correlation between the terrestrial and shallow-marine components of the Sunnyside Member; GPS = Grassy parasequence; SPS = Sunnyside parasequence; IVF = incised-valley fill; OTZ = offshore transition zone; PSB = parasequence boundary; MFS = maximum flooding surface.]()
![(A) Correlation panel showing 29 outcrop logs through the Sunnyside Member and equivalent marginal- to nonmarine deposits; Mb = Member; PS = parasequence; OTZ = offshore transition zone; IVF = incised-valley fill. The total depositional dip extent of the section is approximately 50 km (31 mi). (B) Map of the study area (see Figure 2 for location) showing the location of the measured sections in (A) in relation to the outline of the Book Cliffs and nearby towns and roads. The margins of the incised-valley fills mapped by Howell and Flint (2003) are also shown.]()
![(A) Correlation panel showing 29 outcrop logs through the Sunnyside Member and equivalent marginal- to nonmarine deposits; Mb = Member; PS = parasequence; OTZ = offshore transition zone; IVF = incised-valley fill. The total depositional dip extent of the section is approximately 50 km (31 mi). (B) Map of the study area (see Figure 2 for location) showing the location of the measured sections in (A) in relation to the outline of the Book Cliffs and nearby towns and roads. The margins of the incised-valley fills mapped by Howell and Flint (2003) are also shown.]()
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![Examples of depositional elements in the shallow-marine deposits in the Beckwith Plateau. See Figure 6 for location of images. (a) Wave-dominated delta front in the Kenilworth K4 parasequence. Characterized by gently dipping clinoforms (arrows). Note also the planar interbedded sandstone-, carbonaceous shale- and coal-beds in the lagoonal deposits (CP/L) on top of the shoreface. (b) Shoreface deposit in the Kenilworth K4 parasequence, underlain by erosive offshore transition-zone deposits (OTZe). Note the approximately 3 m-wide, 1 m-deep gutter casts (arrows). (c) Shoreface of the Grassy G1 parasequence, overlying the Sunnyside coal (black arrow) and the Sunnyside incised valley. (d) Near landwards pinch-out of Grassy 2 parasequence. The shoreface of the Grassy 2 contains abundant clinoforms. Note also the distributary channel in the Grassy 1, eroding the bedset boundary. (e) Mudstone-filled subaqueous channel (SC) eroding into the top of the Kenilworth K3 parasequence. (f) Subaqueous channel in the Kenilworth K4 parasequence. Probable lateral accretion surfaces are highlighted by filled and unfilled arrows.]()
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![A, B) grain-size variations in the Ferron Sandstone in the Last Chance Delta and C) in the Notom Delta. In Parts A, B, Ci, and Cii vertical bars represent logged sections through individual depositional elements, with colors showing the associated proportions of each grain-size fraction. In Part Ciii the bars reflect area proportions derived from a 2D cross section, and in Part Civ they record the proportions of facies on the logs that support Figure 10. Similar depositional elements and facies are grouped together and arranged (broadly) into proximal (left) to distal (right) order. Unique numbers at the top each column enable discussion in the text and comparison with Figure 21, where the data are redisplayed by stratigraphy. Numbers at the base of each column reflect the thickness of section for which the grain-size proportions are presented. In Parts A and B: I70, Interstate 70; SMC, South Muddy Creek; PiFl, Picture Flats; CR, Cedar Ridge; FC, fluvial channel; DC, distributary channel; DCh Belt, distributary channel belt; W, F, T, wave, fluvial and tide-dominated “shorelines”; BB, brackish bay, and CS, crevasse splay. The data are derived from Garrison and van den Bergh (2004), van den Bergh and Garrison (2004), and Barton et al. (2004). In Part Ci, IVF, incised-valley fill. In Part Cii: DC, distributary channel; mbc, mouth-bar complex; dla, delta lobe abandonment, and F, F(w), and Fw reflect fluvially dominated delta-front successions. In Part Ciii: TDC, terminal distributary channels; FMB, frictional mouth bar; IMB, inertial mouth bar; FS, frontal splay, and PF, pro-delta. Finally, in Part Civ: FC, fluvio-distributary channel; Fsst, fluvio-distributary sandstones that are not clearly channelized; FldPln, floodplain; ByHd, bayhead delta; ByFl, bayfill; Brs/Inlts, bars/inlets; Fshr, foreshore; USF, upper shoreface; LSF, lower shoreface; OTZ, offshore transition zone; TDC, terminal distributary channel; DF, delta front; PD, prodelta, and SM, shelf mudstone.]()
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Schematic chronostratigraphic chart to show the spatial and temporal correl... Available to Purchase
in High-resolution sequence-stratigraphic correlation between shallow-marine and terrestrial strata: Examples from the Sunnyside Member of the Cretaceous Blackhawk Formation, Book Cliffs, eastern Utah
> AAPG Bulletin
Published: 01 July 2006
Figure 9 Schematic chronostratigraphic chart to show the spatial and temporal correlation between the terrestrial and shallow-marine components of the Sunnyside Member; GPS = Grassy parasequence; SPS = Sunnyside parasequence; IVF = incised-valley fill; OTZ = offshore transition zone; PSB
Image
(A) Correlation panel showing 29 outcrop logs through the Sunnyside Member ... Available to Purchase
in High-resolution sequence-stratigraphic correlation between shallow-marine and terrestrial strata: Examples from the Sunnyside Member of the Cretaceous Blackhawk Formation, Book Cliffs, eastern Utah
> AAPG Bulletin
Published: 01 July 2006
Figure 3 (A) Correlation panel showing 29 outcrop logs through the Sunnyside Member and equivalent marginal- to nonmarine deposits; Mb = Member; PS = parasequence; OTZ = offshore transition zone; IVF = incised-valley fill. The total depositional dip extent of the section is approximately 50 km
Image
(A) Correlation panel showing 29 outcrop logs through the Sunnyside Member ... Available to Purchase
in High-resolution sequence-stratigraphic correlation between shallow-marine and terrestrial strata: Examples from the Sunnyside Member of the Cretaceous Blackhawk Formation, Book Cliffs, eastern Utah
> AAPG Bulletin
Published: 01 July 2006
Figure 3 (A) Correlation panel showing 29 outcrop logs through the Sunnyside Member and equivalent marginal- to nonmarine deposits; Mb = Member; PS = parasequence; OTZ = offshore transition zone; IVF = incised-valley fill. The total depositional dip extent of the section is approximately 50 km
Journal Article
Sedimentology and reservoir properties of tabular and erosive offshore transition deposits in wave-dominated, shallow-marine strata: Book Cliffs, USA Available to Purchase
Journal: Petroleum Geoscience
Publisher: Geological Society of London
Published: 20 January 2015
Petroleum Geoscience (2015) 21 (1): 55–73.
... ) Shoreface deposit in the Kenilworth K4 parasequence, underlain by erosive offshore transition-zone deposits (OTZe). Note the approximately 3 m-wide, 1 m-deep gutter casts (arrows). ( c ) Shoreface of the Grassy G1 parasequence, overlying the Sunnyside coal (black arrow) and the Sunnyside incised valley. ( d...
FIGURES
Journal Article
High-Paleolatitude Environmental Change During the Early To Middle Devonian: Insights from Emsian–Eifelian (Lower–Middle Devonian) Siliciclastic Depositional Systems of the Ceres Subgroup (Bokkeveld Group) of South Africa Available to Purchase
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
Published: 18 September 2018
Journal of Sedimentary Research (2018) 88 (9): 1040–1075.
... associations A–D represent deposits akin to those from storm- and wave- dominated shallow marine depositional systems and respectively comprise offshore (Os), offshore transition zone to distal lower shoreface (OTZ-dLSF), proximal lower shoreface (pLSF), and upper shoreface–beach (USF-beach) paleoenvironments...
FIGURES
Image
Examples of depositional elements in the shallow-marine deposits in the Bec... Available to Purchase
in Sedimentology and reservoir properties of tabular and erosive offshore transition deposits in wave-dominated, shallow-marine strata: Book Cliffs, USA
> Petroleum Geoscience
Published: 20 January 2015
sandstone-, carbonaceous shale- and coal-beds in the lagoonal deposits (CP/L) on top of the shoreface. ( b ) Shoreface deposit in the Kenilworth K4 parasequence, underlain by erosive offshore transition-zone deposits (OTZe). Note the approximately 3 m-wide, 1 m-deep gutter casts (arrows). ( c ) Shoreface
Journal Article
Eifelian–Givetian (Middle Devonian) high-paleolatitude storm- and wave-dominated shallow-marine depositional systems from the Bidouw Subgroup (Bokkeveld Group) of South Africa Available to Purchase
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
Published: 27 November 2019
Journal of Sedimentary Research (2019) 89 (11): 1140–1170.
... of the deposits of offshore (Os), offshore transition zone to distal lower shoreface (OTZ-dLSF), proximal lower shoreface (pLSF), and upper shoreface–beach (USF-Beach) paleoenvironments. These paleoenvironments are arranged as several T-R-controlled storm- and wave-dominated shallow-marine depositional systems...
FIGURES
Journal Article
Sedimentological parameterization of shallow-marine reservoirs Available to Purchase
Journal: Petroleum Geoscience
Publisher: Geological Society of London
Published: 01 February 2008
Petroleum Geoscience (2008) 14 (1): 17–34.
... direction (i.e. a profile from onshore to offshore), the top of the delta plain is essentially flat, the shoreface and OTZ exhibit a dip, typically of 1–2° that decreases into the offshore ( Hampson & Storms 2003 ; Hampson & Howell 2005 ). In a depositional strike direction (i.e. along...
FIGURES
Journal Article
Recycling of Amazon floodplain sediment quantified by cosmogenic 26 Al and 10 Be Available to Purchase
Journal: Geology
Publisher: Geological Society of America
Published: 01 May 2011
Geology (2011) 39 (5): 467–470.
.... , 1998 , 10 Be and 26 Al production rates deduced from an instantaneous event within the dendro-calibration curve, the landslide of Kofels, Otz Valley, Austria : Earth and Planetary Science Letters , v. 161 , p. 231 – 241 , doi: 10.1016/S0012-821X(98)00153-8 . Lal D. , 1991 , Cosmic...
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Journal Article
Notopahar Granitic Complex: An Example of Magmatic Differentiation from Mayurbhanj District, Orissa Available to Purchase
Publisher: Geological Society of India
Published: 01 February 1982
Jour. Geol. Soc. India (1982) 23 (2): 53–66.
... is reaso.nable·. On Q-Ab-Or diagram (Fig. 5) the plo.ts o.f the fo.ur rocks difine a distinct trend o.f increasing Or and Q. One o.f the samples (Sp. no.. 45) oversteps the limit o.f the Bo.wen's Thermal Valley to.wards the Or-rich side ;-this NOTOPAHAR GRANITIC COMPLEX 59 Figure 4A. Photomicrograph of quartz...
Journal Article
PUBLICATIONS RECEIVED Available to Purchase
Journal: Geological Magazine
Publisher: Cambridge University Press
Published: 01 March 2007
Geological Magazine (2007) 144 (2): 415.
... otze , H.-J., R amos , V. A., S trecker , M. R. & W igger , P. (eds) 2006. The Andes. Active Subduction Orogeny . Frontiers in Earth Sciences Series. xxii + 569 pp. + CD-ROM. Berlin, Heidelberg, Dordrecht: Springer-Verlag. Price Euros 149.95, US $189.00, £115.50 (hard covers). ISBN 9783 540 24329...
Journal Article
High-resolution sequence-stratigraphic correlation between shallow-marine and terrestrial strata: Examples from the Sunnyside Member of the Cretaceous Blackhawk Formation, Book Cliffs, eastern Utah Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 July 2006
AAPG Bulletin (2006) 90 (7): 1121–1140.
...Figure 9 Schematic chronostratigraphic chart to show the spatial and temporal correlation between the terrestrial and shallow-marine components of the Sunnyside Member; GPS = Grassy parasequence; SPS = Sunnyside parasequence; IVF = incised-valley fill; OTZ = offshore transition zone; PSB...
FIGURES
Journal Article
Common Spring Types in the Valley and Ridge Province: There Is More than Karst Available to Purchase
Published: 06 July 2020
Environmental & Engineering Geoscience (2020) 26 (3): 345–358.
...Dorothy J. Vesper; Ellen K. Herman ABSTRACT The Valley and Ridge Province (V&R) of the central Appalachians is rich in springs that support ecosystems, provide local water resources, and export water from the region. Although there has been extensive research on springs in the province...
Image
A , B) grain-size variations in the Ferron Sandstone in the Last Chance D... Available to Purchase
in “Grain-size bookkeeping,” a new aid for siliciclastic systems with examples from paralic environments
> Journal of Sedimentary Research
Published: 28 October 2019
Bergh (2004) , van den Bergh and Garrison (2004) , and Barton et al. (2004) . In Part Ci, IVF, incised-valley fill. In Part Cii: DC, distributary channel; mbc, mouth-bar complex; dla, delta lobe abandonment, and F, F(w), and Fw reflect fluvially dominated delta-front successions. In Part Ciii: TDC
Journal Article
Lithostratigraphy and sedimentology of the Middle Devonian Tra-Tra Formation, including the Grootrivier Member (Bokkeveld Group, Cape Supergroup), South Africa Available to Purchase
Journal: South African Journal of Geology
Publisher: Geological Society of South Africa
Published: 01 September 2020
South African Journal of Geology (2020) 123 (3): 381–398.
.... It comprises three discrete lithofacies associations (termed E-G) which are interpreted as deposits of channelised tidal flat-lagoons, transgressive beach-barriers and wave-influenced prodeltas to distal delta-fronts. They accumulated within a series of incised coastal-plain valley-fill system along...
FIGURES
Journal Article
Early Holocene collapse of Volcán Parinacota, central Andes, Chile: Volcanological and paleohydrological consequences Available to Purchase
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 01 November 2015
GSA Bulletin (2015) 127 (11-12): 1681–1688.
... event within the dendro-calibration curve, the landslide of Köfels, Ötz Valley, Austria : Earth and Planetary Science Letters , v. 161 , p. 231 – 241 , doi:10.1016/S0012-821X(98)00153-8. Kull C. Imhof S. Grosjean M. Zech R. Veit H. , 2008 , Late Pleistocene glaciation...
FIGURES
Journal Article
Phosphoran olivine overgrowths: Implications for multiple impacts to the Main Group pallasite parent body Available to Purchase
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 October 2015
American Mineralogist (2015) 100 (10): 2043–2052.
... gneisses from a prehistoric sacrificial burning site (Ötz Valley, Tyrol, Austria) . European Journal of Mineralogy , 16 , 631 – 640 . Wadhwa M. Srinivanson G. Carlson R.W. ( 2006 ) Timescales of planetesimal differentiation in the early solar system . Meteoritics and the Early Solar...
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Journal Article
Formation of phosphorus-rich olivine in Dar al Gani 978 carbonaceous chondrite through fluid-assisted metamorphism Available to Purchase
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 January 2017
American Mineralogist (2017) 102 (1): 98–107.
... formation of phosphorus-rich olivines in partially molten metapelitic gneisses from a prehistoric sacrificial burning site (Ötz Valley, Tyrol, Austria) . European Journal of Mineralogy , 16 , 631 – 640 . Wang Y. Hua X. Hsu W. ( 2007 ) Petrogenesis of opaque assemblages...
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Journal Article
The triggering of aftershocks by the free oscillations of the earth Available to Purchase
Publisher: Seismological Society of America
Published: 01 April 1996
Bulletin of the Seismological Society of America (1996) 86 (2): 299–305.
....
Tullis
T. E.
(1992) .
The contact between opposing fault surfaces at Dixie Valley, Nevada, and implications for fault mechanics ,
J. Geophys. Res. (Solid) B-11 ,
15425 -
15435 .
Ryall...
Journal Article
Paleoerosion Rates from Cosmogenic 10 Be in a 1.3 Ma Terrace Sequence: Response of the River Meuse to Changes in Climate and Rock Uplift Available to Purchase
Journal: The Journal of Geology
Publisher: The University of Chicago Press
Published: 01 March 2004
The Journal of Geology (2004) 112 (2): 127–144.
... an instantaneous event within the dendro-calibration curve, the landslide of Köfels, Ötz Valley, Austria . Earth Planet. Sci. Lett. 161 : 231 – 241 . Lippolt , H. J. 1983 . Distribution of volcanic activity in space and time . In Fuchs , K. ; von Gehlen , K. ; Maelzer , H...
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