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Robbins Shale Member

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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1963
AAPG Bulletin (1963) 47 (10): 1873–1877.
... to include the Haskell Limestone Member, Robbins Shale Member, Ireland Sandstone Member, Amazonia Limestone Member, and a member to be named in the forthcoming report. The Missourian-Virgilian boundary is placed at the base of the redefined Douglas Group. Fig. 3. —Reclassification of Douglas...
FIGURES
Journal Article
Published: 01 November 2003
Journal of Paleontology (2003) 77 (6): 1195–1197.
... Shale Member of the Cass Limestone in southeastern Kansas. The assemblage from the Little Pawnee Shale at this locality, in addition to Mapesites chautauquaensis n. gen. and sp., includes Neoaganides grahamensis Plummer and Scott, 1937 , Glaphyrites n. sp., Neodimorphoceras texanum...
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Image
—Generalized Pennsylvanian stratigraphic sequence in eastern Kansas. In formation column, capital names denote limestone formations that also name megacyclothems of Moore (1949) and Weller (1958); most now are interpreted to be single transgressive-regressive sequences, thus are considered simply cyclothems; names in lower case are other names applied to similar cyclothems (adapted from Heckel and Baesemann, 1975). Asterisks denote units that have received petrologic study: Excello—James (1970); Altamont—Schenk (1967); Swope—Payton (1966), Mossler (1973); Dennis—Payton (1966), Frost (1975); Wyandotte—Crowley (1969); Plattsburg—Harbaugh (1959; Harbaugh et al, 1965); Stanton and South Bend (separate cycles)—Heckel (1975a, b); Haskell (includes overlying Robbins shale)—Ball (1964, p. 120-140); Oread—Troell (1969), Toomey (1964, 1969a), Evans (1967). Probable correlations of members of Fort Scott and Pawnee Limestones with units in Illinois (Willman et al, 1975, p. 189-191) and Iowa (J. W. Swade, personal commun., 1976) suggest that these formations, which have received little detailed study in Kansas, are more complex than most of those listed here.
Published: 01 July 1977
(1966) , Frost (1975) ; Wyandotte— Crowley (1969) ; Plattsburg— Harbaugh (1959 ; Harbaugh et al, 1965); Stanton and South Bend (separate cycles)— Heckel (1975a , b); Haskell (includes overlying Robbins shale)— Ball (1964 , p. 120-140); Oread— Troell (1969) , Toomey (1964 , 1969a ), Evans (1967
Book Chapter

Author(s)
Clive R. Calver
Series: Geological Society, London, Memoirs
Published: 01 January 2011
DOI: 10.1144/M36.64
EISBN: 9781862394117
... uncertainties) to the 643± 2 Ma Re–Os age for the Sturtian post-glacial Tindelpina Shale Member ( Kendall et al. 2006 ). The rhyodacite underlying the Croles Hill Diamictite at Robbins Passage has been dated by U–Pb (SHRIMP on zircon) at 582.1± 4.1 Ma ( n =46, MSWD=0.94, precision limits at 95% (2σ...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 04 April 2024
GSA Bulletin (2024) 136 (9-10): 4285–4300.
..., Lake Huron ( Kolak et al., 1999 ; Hoaglund et al., 2004 ), southern Lake Huron ( Robbins, 1980 ), and western Lake Erie ( Nriagu and Dell, 1974 ; Haack et al., 2005 ). TABLE 1. GREAT LAKES PORE-WATER CHEMISTRY DATA SETS USED IN THIS STUDY Benthic sediment pore-water chemistry can...
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Journal Article
Journal: GSA Bulletin
Published: 06 July 2022
GSA Bulletin (2023) 135 (3-4): 753–766.
...-rich shale interbedded with Mn-rich carbonates that is commonly interpreted as deep subtidal deposits ( Fig. 3A ; Fang et al., 2020 ). The upper Member II in the Yanqing area contains Mn-bearing dolostone with microbially induced cracks that are indicative of intertidal to supratidal deposition ( Figs...
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Journal Article
Journal: GSA Bulletin
Published: 06 November 2023
GSA Bulletin (2024) 136 (7-8): 2735–2752.
...Zhiquan Li; Kurt O. Konhauser; Yongzhang Zhou; Erin Adlakha; Mark Button; Cody Lazowski; Ernesto Pecoits; Natalie R. Aubet; Pilar Lecumberri-Sanchez; Daniel S. Alessi; Leslie J. Robbins Abstract Trace metal and rare earth element (REE) abundances in banded iron formations are critical for assessing...
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Journal Article
Published: 01 April 2024
American Mineralogist (2024) 109 (4): 764–784.
..., and Liujiagou sections can be divided into two members, the lower Daizhuangzi (DZZ) and upper Laohuding (LHD) members ( Fig. 2e ). The DZZ Member (~153 m) is a set of manganiferous dolomites with thin-beds of intercalated manganiferous and potassium-rich shales. The overlying LHD Member (~181 m) comprises...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1995
AAPG Bulletin (1995) 79 (7): 1019–1042.
... and Swineford, 1957 ). This zone correlates with the Little Pawnee Shale Member of the Cass Limestone in Nebraska, which consists of a phosphatic, platy black shale ( Ball, 1981 ). In Kansas, the dark, phosphatic shale grades upward into the gray shales of the Robbins Shale that contain a sparse normal-marine...
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Journal Article
Journal: Palynology
Published: 02 October 2018
Palynology (2018) 42 (4): 438–456.
... the Corbula bed and the Thorp Spring Member. Most are from marly saltmarsh shales, namely beds 7–8 (79-21, 79-22, 79-23, 79-24) and 11 (79-20) of Perkins ( 1979 ) at Barker Branch, and beds 4 (79-25) and 8 (79-26, 79-27, 79-28) of Nagle ( 1968 ) at Cedar Brake Camp. Nagle's bed 4 represents the saltmarsh...
Journal Article
Journal: GSA Bulletin
Published: 20 December 2017
GSA Bulletin (2018) 130 (5-6): 941–951.
... tied to another form of microbial respiration, such as methanogenesis ( Konhauser et al., 2005 ), or it would have been buried in carbon-rich oxidant-poor sediments, such as black shales. Peak iron deposition in the Dales Gorge Member is estimated at 4.38 × 10 13 g or 7.85 × 10 11 mol of Fe yr –1...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1979
AAPG Bulletin (1979) 63 (1): 87–105.
... in the deposition of a predominantly sandstone unit, the Logan Canyon Formation. Two major shale tongues, the Naskapi Member and the Sable Member, are present in the Logan Canyon Formation. The Naskapi ranges from 0 to 305 m (0 to 1,000 ft). It is brown, brownish-gray, or green-gray shale, and near the base...
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Journal Article
Published: 01 July 2019
American Mineralogist (2019) 104 (7): 917–928.
... sedimentary records of metal availability are necessary for constraining the availability of metals ( Robbins et al. 2016 ). As with modern sediments discussed above, the bulk rock inventory or trace metals in shales deposited throughout Earth's history is useful for informing general metal availability...
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Journal Article
Journal: GSA Bulletin
Published: 11 April 2025
GSA Bulletin (2025)
... members. Member I primarily consists of manganese-rich dolostone and thin green shale interbeds with hummocky bedding at the Jixian, Chengde, and Kuancheng sections (Figs. 2A 2C), with locally developed sedimentary manganese deposits along the northeastern margin of the Yanliao Basin (Yan et al., 2024...
Journal Article
Published: 01 March 1965
Bulletin of Canadian Petroleum Geology (1965) 13 (1): 195.
...B. P. Robbins Provenance, depositional environment and paleoecology of the Imperial Formation were determined by means of a petrological and palaeontological study of four sections in the northeastern Mackenzie Mountains. The principal source for these rocks was sedimentary and low-rank metamorphic...
Journal Article
Published: 01 July 2006
Journal of the Geological Society (2006) 163 (4): 587–594.
... , M. , 1982 . Palynologic study of the Cretaceous sediments of Douha mez, eastern Bohemia . Casopis pro Mineralogii a Geologii , 27 ( 1 ), 85 – 93 . Wingate , F.H. , 1980 . Plant microfossils from the Denton Shale Member of the Bokchito Formation (Lower Cretaceous, Albian...
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Journal Article
Published: 30 March 2022
Geological Magazine (2022) 159 (6): 963–980.
... and exhibit a maximum thickness of c. 7000 m. The Palaeogene strata include the Kongdian, Shahejie (Es) and Dongying formations from bottom to top (Fig.  2 ). The Es Formation can be divided into four members (Es1–Es4; Fig.  2 ; Yang et al. 2018 ). The upper member of Es4 (Es4s) shale is carbonate-rich...
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Series: AAPG Memoir
Published: 01 January 2012
DOI: 10.1306/13321469M97948
EISBN: 9781629810119
..., formation thickness, underlying salt movement or dissolution, and level of thermal maturity and oil-generation capacity of Bakken source rocks. The Bakken Formation consists of three informal members: (1) lower shale member; (2) middle sandstone member; and (3) upper shale member. Shale members are rich...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1975
AAPG Bulletin (1975) 59 (9): 1529–1548.
...W. J. Perry; J. P. Minard; E. G. A. Weed; E. I. Robbins; E. C. Rhodehamel Abstract A synthesis of studies of sea-floor outcrops of the sedimentary wedge beneath the northeastern United States continental shelf and slope and a reassessment of coastal plain Mesozoic stratigraphy, particularly...
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Journal Article
Journal: Geosphere
Published: 01 December 2016
Geosphere (2016) 12 (6): 1744–1773.
... on informal sand packet designations ( Nicholson, 1980 ) are shown for each well, and the map distribution of the well sites is shown on the Figure 1 inset map. Distinct silt and silty shale-bounded sand units within the Kern River Formation, as identified by log and core data ( Robbins, 2014 ), were...
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