2019
DOI: 10.1007/978-3-030-11295-0_4
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The Late Triassic–Middle Jurassic Passive Margin Stage

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Cited by 8 publications
(6 citation statements)
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“…Middle Jurassic sedimentation in the eastern margin of Iberia took place on a carbonate-platform system in which the accumulation rate, thickness and lithofacies were controlled by a grid of NW and NE active faults. These faults differentiated blocks with variable subsidence rates conforming paleogeographic highs and depocenters, as well as internal and external platform facies types (Fernández-López & Gómez, 1990Gómez & Fernández-López, 2004aGarcía-Frank, 2006;García-Frank et al, 2006, 2008Gómez et al, 2019) (Fig. 1B).…”
Section: Introductionmentioning
confidence: 98%
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“…Middle Jurassic sedimentation in the eastern margin of Iberia took place on a carbonate-platform system in which the accumulation rate, thickness and lithofacies were controlled by a grid of NW and NE active faults. These faults differentiated blocks with variable subsidence rates conforming paleogeographic highs and depocenters, as well as internal and external platform facies types (Fernández-López & Gómez, 1990Gómez & Fernández-López, 2004aGarcía-Frank, 2006;García-Frank et al, 2006, 2008Gómez et al, 2019) (Fig. 1B).…”
Section: Introductionmentioning
confidence: 98%
“…After the Permian-Triassic rifting interval, Iberia evolved into a passive margin stage from the latest Triassic until the end of the Middle Jurassic. Meanwhile, active rifts were taking place both in the west (leading to the onset of spreading in the northern part of the Central Atlantic Ocean), and in the south and east (resulting in the generation of the Ligurian and Alpine Tethys Oceans) of Iberia (Gómez et al, 2019) (Fig. 1).…”
Section: Introductionmentioning
confidence: 99%
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