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Astronomical time calibration of the Upper Devonian Lali section, South China
, 2020The Late Devonian Period was a critical geological interval, affected by numerous significant global bio- and environmental events, including the Kellwasser, annulata and Hangenberg events, and a major climate transition leading to the Carboniferous ice ...
Kunyuan Ma +3 more
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American Association of Petroleum Geologists Bulletin, 2019
The influence of thermal maturity on porosity in shale samples from the Upper Devonian Duvernay Formation is examined. The samples span a maturity range from immature to the wet gas window.
T. Dong +5 more
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The influence of thermal maturity on porosity in shale samples from the Upper Devonian Duvernay Formation is examined. The samples span a maturity range from immature to the wet gas window.
T. Dong +5 more
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Science, 1967
We present evidence proving the existence of seeds in the Upper Devonian and extending the known age of seed plants from the Lower Carboniferous (Mississippian) into the Upper Devonian.
J M, Pettitt, C B, Beck
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We present evidence proving the existence of seeds in the Upper Devonian and extending the known age of seed plants from the Lower Carboniferous (Mississippian) into the Upper Devonian.
J M, Pettitt, C B, Beck
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Memoir 120: Mudstone Diagenesis: Research Perspectives for Shale Hydrocarbon Reservoirs, Seals, and Source Rocks, 2019
Organic matter (OM) in petroleum source rocks is a mixture of organic macerals that follow their own specific evolutionary pathways during thermal maturation.
Bei Liu, J. Schieber, M. Mastalerz
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Organic matter (OM) in petroleum source rocks is a mixture of organic macerals that follow their own specific evolutionary pathways during thermal maturation.
Bei Liu, J. Schieber, M. Mastalerz
semanticscholar +1 more source
Sedimentary Geology, 2018
We present a model for organic carbon accumulation in the Upper Devonian Duvernay Formation of the Western Canada Sedimentary Basin, relating total organic carbon (TOC) concentrations to a high resolution geochemical and organic petrologic database and ...
N. Harris +3 more
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We present a model for organic carbon accumulation in the Upper Devonian Duvernay Formation of the Western Canada Sedimentary Basin, relating total organic carbon (TOC) concentrations to a high resolution geochemical and organic petrologic database and ...
N. Harris +3 more
semanticscholar +1 more source
, 2020
The Devonian flora comprises abundant both endemic and widely-distributed plants and witnessed the earliest phytogeographical differentiation. One of the best studied Devonian plants, the protolepidodendralean lycopsid Leclercqia, was known to be widely ...
Honghe Xu +7 more
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The Devonian flora comprises abundant both endemic and widely-distributed plants and witnessed the earliest phytogeographical differentiation. One of the best studied Devonian plants, the protolepidodendralean lycopsid Leclercqia, was known to be widely ...
Honghe Xu +7 more
semanticscholar +1 more source
Diagenetic evolution of the upper Devonian phosphorites, Alborz Mountain Range, northern Iran
Sedimentary Geology, 2018The upper Devonian, mixed siliciclastic‑carbonate stratigraphic succession of the Geirud Formation in the Alborz Mountain Range, north of Iran, hosts numerous phosphorites and phosphatic rocks. These phosphorites, which represent one of the most globally
W. Salama +3 more
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Palaeogeography, Palaeoclimatology, Palaeoecology, 2018
Late Devonian terrestrial floodplain environments were important sites of plant and animal diversification and evolution. Recently discovered fossil sites in the Catskill Formation in north-central Pennsylvania yield important insights into Late Devonian
D. Broussard +5 more
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Late Devonian terrestrial floodplain environments were important sites of plant and animal diversification and evolution. Recently discovered fossil sites in the Catskill Formation in north-central Pennsylvania yield important insights into Late Devonian
D. Broussard +5 more
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Summary of Upper Devonian Stratigraphy
American Midland Naturalist, 1935The Upper Devonian terrane of New York and adjoining regions consists of many thousands of feet of clastic deposits, in the east or southeast, thinning down to but a few hundred feet at the west or northwest. Beds which are coarse sandstones, or conglomerates, at the east, grade westward into shales that grow continually finer until at length they ...
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