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Aglegal Member

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Tetrapod footprints from the <b>Aglegal</b> <b>Member</b> (T4) of the Timezgadiouine Form...
in > PALAIOS
Published: 01 September 2011
TABLE 2 Tetrapod footprints from the Aglegal Member (T4) of the Timezgadiouine Formation defined by maximum pes length, generalized pes imprint morphology, and potential trackmakers (adapted from Klein et al., 2011 ).
Journal Article
Journal: PALAIOS
Published: 01 September 2011
PALAIOS (2011) 26 (9): 555–566.
...TABLE 2 Tetrapod footprints from the Aglegal Member (T4) of the Timezgadiouine Formation defined by maximum pes length, generalized pes imprint morphology, and potential trackmakers (adapted from Klein et al., 2011 ). ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1980
AAPG Bulletin (1980) 64 (7): 988–1003.
.... Throughout most of this extent it lies with angular unconformity on eroded beds of the Tourbian member. In the vicinity of Iferd and 4 km south of Timesgadiouine, it lies on truncated beds of the Driss River conglomerates. The Tanameurt is conformably overlain by the Aglegal sandstone. Although...
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Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.265.01.14
EISBN: 9781862395138
..., and the intercalated clayey-silty layers are dark red-brown. Above an erosional unconformity, the El Menizla Formation is overlain by Late Triassic sediments of the Timesgadiouine Formation (T5 or Irohalene Member). Modern elements of the flora, such as Culmitzschia, Lodevia and Feysia, give an Autunian, Early...
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