1997
DOI: 10.1016/s0743-9547(97)00036-6
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Devonian fluviodeltaic sedimentation in Hong Kong

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Cited by 5 publications
(6 citation statements)
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“…Based on the collected LepidodendropsisBothriolepis assemblage, the Van Huong Formation was considered to be Middle Devonian (Givetian, see Long et al, 1990) in age, and overlying massive sandstones may also extend into the early Late Devonian (Janvier et al, 2003). The overall sedimentary record mainly represents fluvial to deltaic prograding deposits close to a shoreline and are very similar to deposits of the same age known from South China (Xun et al, 1996;Jones et al, 1997). The Devonian red-coloured sediments are found in the Hue area while marine sediments of the same age are found in the west, in the center of the Red River Basin.…”
Section: Geological Settingsupporting
confidence: 63%
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“…Based on the collected LepidodendropsisBothriolepis assemblage, the Van Huong Formation was considered to be Middle Devonian (Givetian, see Long et al, 1990) in age, and overlying massive sandstones may also extend into the early Late Devonian (Janvier et al, 2003). The overall sedimentary record mainly represents fluvial to deltaic prograding deposits close to a shoreline and are very similar to deposits of the same age known from South China (Xun et al, 1996;Jones et al, 1997). The Devonian red-coloured sediments are found in the Hue area while marine sediments of the same age are found in the west, in the center of the Red River Basin.…”
Section: Geological Settingsupporting
confidence: 63%
“…Depositional facies settings of Late and Middle Devonian siliciclastics in NE Vietnam are comparable to those along the southeastern coast of China (e.g. Jones et al, 1997) and they also yield the same vertebrate remains (Yang et al, 1981;Lee, 1991;Jones et al, 1997;Janvier et al, 2003). In this paper, we present U-Pb detrital zircon ages of siliciclastic rocks from two formations in NE Vietnam and discuss the results with paleo(bio)geographic affinities and derivations of Devonian siliciclastics in southern China.…”
Section: Introductionmentioning
confidence: 85%
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“…15°) and generally non-metamorphosed. Devonian rocks NW of the TCF contain an Early to Middle Devonian flora and marine fauna, and show paleocurrent directions toward the northwest (Jones et al, 1997). In contrast, Devonian rocks to the south have a Late Devonian flora and show paleocurrent directions toward the southeast (Jones et al, 1997).…”
Section: Geological Settingmentioning
confidence: 99%
“…Devonian rocks NW of the TCF contain an Early to Middle Devonian flora and marine fauna, and show paleocurrent directions toward the northwest (Jones et al, 1997). In contrast, Devonian rocks to the south have a Late Devonian flora and show paleocurrent directions toward the southeast (Jones et al, 1997). Jurassic sandstones and shales north of the TCF have an Early to Middle Jurassic terrestrial flora and marine fauna , whereas Jurassic sandstones and shales south of the TCF are exclusively marine .…”
Section: Geological Settingmentioning
confidence: 99%