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La Rellana-Ricardillo Field

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Image
Quantitative relative sea level curve for the <b>La</b> <b>Rellana</b>-<b>Ricardillo</b> <b>field</b> a...
Published: 01 November 2013
Figure 18 Quantitative relative sea level curve for the La Rellana-Ricardillo field area based on pinning points. See Figure 15 for location of pinning points. La Rellana-Ricardillo field area. Minimum amplitudes range between 57.8 and 76.6 m (189.6 and 251.3 ft).
Image
Fence diagram for the <b>La</b> <b>Rellana</b>-<b>Ricardillo</b> <b>field</b> area displaying the distr...
Published: 01 November 2013
Figure 14 Fence diagram for the La Rellana-Ricardillo field area displaying the distribution and geometries of lithofacies. Sequences drape paleotopography and maintain relatively uniform thickness across the area with oolite dominant. Porites boundstone in sequence 3 is laterally extensive
Image
Cross-section of the <b>La</b> <b>Rellana</b>-<b>Ricardillo</b> <b>field</b> area. Inset shows topograp...
Published: 01 November 2013
Figure 15 Cross-section of the La Rellana-Ricardillo field area. Inset shows topographic map; white outline encloses area where stratigraphic sections were measured to build the cross section. Pinning points (PP) are used to construct the sea level curve of Figure 18 . Thrombolite boundstone
Image
(A) Location map of Neogene basins within the Betic Cordillera of southern ...
Published: 01 November 2013
Figure 1 (A) Location map of Neogene basins within the Betic Cordillera of southern Spain. Modified from Gibbons and Moreno (2003) . (B) Generalized geologic map of the Cabo de Gata region and location of the La Molata and La Rellana-Ricardillo field areas with the Carboneras fault to the west
Image
(A) Location map of Neogene basins within the Betic Cordillera of southern ...
Published: 01 November 2013
Figure 1 (A) Location map of Neogene basins within the Betic Cordillera of southern Spain. The red box outlines the Cabo de Gata volcanic province. Modified from Gibbons and Moreno (2003) . (B) Generalized geologic map of the Cabo de Gata region and location of the La Molata and La Rellana
Image
Topographic map, showing present-day elevations, with paleogeographic infor...
Published: 01 November 2013
Rellana-Ricardillo field area encompasses an elongate area, 1.63 × 0.93 km (1.01 × 0.58 mi) at its widest point. The basal TCC surface crops out between 181 and 257 m (594 and 843 ft) elevation, with the highest TCC outcrop at 269 m (883 ft). Volcanic highs are to the northwest and west. The Agua Amarga
Image
Lithofacies photographs for the beach sequence in sequence 1 at <b>La</b> <b>Rellana</b>-...
Published: 01 November 2013
Figure 8 Lithofacies photographs for the beach sequence in sequence 1 at La Rellana-Ricardillo. Field scale is marked in centimeter increments with black and white bars. (A) Beach sequence with bioturbate ooid grainstone (BOG) transitions upward to trough cross-bedded ooid grainstone (TCOG
Journal Article
Journal: AAPG Bulletin
Published: 01 November 2013
AAPG Bulletin (2013) 97 (11): 1997–2034.
...Figure 18 Quantitative relative sea level curve for the La Rellana-Ricardillo field area based on pinning points. See Figure 15 for location of pinning points. La Rellana-Ricardillo field area. Minimum amplitudes range between 57.8 and 76.6 m (189.6 and 251.3 ft). ...
FIGURES | View All (19)
Journal Article
Journal: AAPG Bulletin
Published: 01 November 2013
AAPG Bulletin (2013) 97 (11): 2035–2057.
...Figure 1 (A) Location map of Neogene basins within the Betic Cordillera of southern Spain. The red box outlines the Cabo de Gata volcanic province. Modified from Gibbons and Moreno (2003) . (B) Generalized geologic map of the Cabo de Gata region and location of the La Molata and La Rellana...
FIGURES | View All (11)
Image
Fence diagrams of the resulting reservoir analog models from <b>La</b> Molata (A–C...
Published: 01 November 2013
the field area. This is partially caused by depositional facies distributions, but it is also the result of diagenesis. At the southern margin of La Rellana, low porosities in sequence 3 occur in the coral reefs. (F) Permeability distribution in La Rellana-Ricardillo. Permeability is also heterogeneous
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Base of the TCC surface (<b>La</b> Molata on left and <b>La</b> <b>Rellana</b>-<b>Ricardillo</b> on rig...
Published: 01 November 2013
Figure 6 Base of the TCC surface (La Molata on left and La Rellana-Ricardillo on right) created in the models is shown here with the measured sections (red sticks) and pseudosections (white sticks) displayed. Sections were commonly spaced less than 10 m (33 ft) apart to constrain the geometry
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Comparison of the photomosaic mapped in the <b>field</b> with the lithofacies mode...
Published: 01 November 2013
) Southern margin of La Rellana-Ricardillo where coral reefs are laterally continuous and thick at the lowest elevations in sequence 3. Sequence 2 thrombolites are laterally extensive and interbedded with oolites high in the section. Note absence of microbialites in sequence 1 with only beach lithofacies
Journal Article
Published: 01 October 2014
Italian Journal of Geosciences (2014) 133 (3): 325–340.
... ). The Ricardillo Formation is exposed to the northeast of Las Negras along inland and coastal exposures (S1). It consists of columnar jointed coherent lavas that form tabular bodies dipping shallowly to the north. Lavas are dacitic and porphyritic, with feldspar, plagioclase, pyroxene, amphibole, quartz...
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Journal Article
Published: 01 July 2012
Journal of Sedimentary Research (2012) 82 (7): 499–520.
...) that subdued topography in one area to produce a ramp-like surface, but did not significantly infill a large paleovalley located in another area. Further relative rise in sea level resulted in an extensive reefal platform that formed along a paleo-high adjacent to both features (La Rellana platform...
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Journal Article
Published: 01 May 2004
Journal of the Geological Society (2004) 161 (3): 387–399.
... Ricardillo area in the Cabo de Gata region formed at the foot of rocky submarine cliffs ( Betzler et al . 2000 ). In the northernmost section (the Espolón de la Quesería section), the transgressive middle unit sediments display gentle, homoclinal ramp geometries. Rudstones (grainstones) alternate...
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