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32 results for “geological formations”
Text-fig. 1. a: Idealised section of the Intra-Sudetic Basin (from Opluštil et al. 2016); b: Geological sketch map of the IntraSudetic Basin, here simplified (after Prouza and Tásler 2001, Pešek 2004). Explanations: 1 – Bohdašín Formation (Triassic), 2 – Bohuslavice Formation (Thuringian), 3 – Trutnov Formation (Saxonian), 4–13 Broumov Formation (Autunian): 4 – Martínkovice Member, 5 – Martínkovice Member with Jetřichovice, Hejtmánkovice and Vižňov horizons, 6–13 – Olivětín Member: 6 – Walchia bone coal facies, 7 – Basaltoides of the Šonov Group, 8 – Volcanoclastic facies, 9 – Aleuropelites, 10 – Ignimbrites, 11 – Rhyolite tuffs, 12 – Ruprechtice Limestone Horizon, 13 – Otovice Limestone Horizon. Localities: O1 – Otovice "Černý potok", O2 – Otovice "Stěnava", O3 – Otovice "Chmelnice", O4 – Otovice "Vápenka", R1 – Ruprechtice "Vápencové lomy", R2 – Ruprechtice "Pod Světlinou", R3 – Olivětín "Nad náhonem". in Actinopterygians Of The Broumov Formation (Permian) In The Czech Part Of The Intra-Sudetic Basin (The Czech Republic)
Text-fig. 1. a: Idealised section of the Intra-Sudetic Basin (from Opluštil et al. 2016); b: Geological sketch map of the IntraSudetic Basin, here simplified (after Prouza and Tásler 2001, Pešek 2004). Explanations: 1 – Bohdašín Formation (Triassic), 2 – Bohuslavice Formation (Thuringian), 3 – Trutnov Formation (Saxonian), 4–13 Broumov Formation (Autunian): 4 – Martínkovice Member, 5 – Martínkovice Member with Jetřichovice, Hejtmánkovice and Vižňov horizons, 6–13 – Olivětín Member: 6 – Walchia bone coal facies, 7 – Basaltoides of the Šonov Group, 8 – Volcanoclastic facies, 9 – Aleuropelites, 10 – Ignimbrites, 11 – Rhyolite tuffs, 12 – Ruprechtice Limestone Horizon, 13 – Otovice Limestone Horizon. Localities: O1 – Otovice "Černý potok", O2 – Otovice "Stěnava", O3 – Otovice "Chmelnice", O4 – Otovice "Vápenka", R1 – Ruprechtice "Vápencové lomy", R2 – Ruprechtice "Pod Světlinou", R3 – Olivětín "Nad náhonem".
Text-fig. 7. Geology of the Muaredzi-Muanza sector of the Cheringoma Plateau showing the location of fossil occurrences. White stars – fossiliferous localities mapped by Pickford (2012, 2013), Black stars – fossil sites mapped by Habermann et al. (2019) and d'Oliveira Coelho et al. (2021) (GPL 12 and GPL 12b correspond to the White Patch sites). TTI – Cheringoma Formation, TTs1 – Mazamba Formation, TTs1a – Palaeopan facies, TTs2 – Inhaminga Formation, Qc – Quaternary sediments. The base map is modified from Google Earth. in Stratigraphy, Chronology And Palaeontology Of The Tertiary Rocks Of The Cheringoma Plateau, Mozambique
Text-fig. 7. Geology of the Muaredzi-Muanza sector of the Cheringoma Plateau showing the location of fossil occurrences. White stars – fossiliferous localities mapped by Pickford (2012, 2013), Black stars – fossil sites mapped by Habermann et al. (2019) and d'Oliveira Coelho et al. (2021) (GPL 12 and GPL 12b correspond to the White Patch sites). TTI – Cheringoma Formation, TTs1 – Mazamba Formation, TTs1a – Palaeopan facies, TTs2 – Inhaminga Formation, Qc – Quaternary sediments. The base map is modified from Google Earth.
Text–fig. 1. Geographical and geological situation in the James Ross Island region. The locality No. 32 and the position of the Johann Gregor Mendel Czech Antarctic Station (JGM) are indicated. Modified from Sakala and Vodrážka (2014). in Marattiopsis Vodrazkae Sp. Nov. (Marattiaceae) From The Campanian Of The Hidden Lake Formation, James Ross Island, Antarctica.
Text–fig. 1. Geographical and geological situation in the James Ross Island region. The locality No. 32 and the position of the Johann Gregor Mendel Czech Antarctic Station (JGM) are indicated. Modified from Sakala and Vodrážka (2014).
Text-fig. 11. Geological map south of the Nel'ma Bay. 1 - granodiorite (Early Palaeogene); 2 – Eocene andesitic and dacitic tuff with plant-bearing argillitic lenses; 3 – Late Eocene to Early Miocene andesite-basalt (Kizi Volcanic Group); 4 – tuffogenous sedimentary plant-bearing lenses with plant fossils; 5 – Dacite neck (Early Oligocene) 1 km south of the Dembi Bay; 6 – Pliocene pebbles and conglomerates; 7 – Plateaubasalts (Sovgavan' Formation, Late Neogene–Quaternary); 8 – Quaternary alluvial deposits; 9 – localities with fossil plants: a – Sonje, b – Bui, c – Dembi. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)
Text-fig. 11. Geological map south of the Nel'ma Bay. 1 - granodiorite (Early Palaeogene); 2 – Eocene andesitic and dacitic tuff with plant-bearing argillitic lenses; 3 – Late Eocene to Early Miocene andesite-basalt (Kizi Volcanic Group); 4 – tuffogenous sedimentary plant-bearing lenses with plant fossils; 5 – Dacite neck (Early Oligocene) 1 km south of the Dembi Bay; 6 – Pliocene pebbles and conglomerates; 7 – Plateaubasalts (Sovgavan' Formation, Late Neogene–Quaternary); 8 – Quaternary alluvial deposits; 9 – localities with fossil plants: a – Sonje, b – Bui, c – Dembi.
Fig. 17 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 17. View looking northeast from Xanadu Southwest showing resistant, vaguely bedded, cross-strata of Facies E-2 in foreground by pack.
Fig. 13 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 13. View looking northeast across low-relief exposures of structureless sandstone (Facies S) at Sugar Mountain, between the Sphinx and Camel Humps.
Fig. 11 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 11. Top: Panoramic view of exposures at Ankylosaur Flats, including bluffs above flats. Sphinx is located just past the right edge of the photo (vehicle near left center for scale). Bottom: Schematic cross section of exposures at Ankylosaur Flats. Location of site is seen on maps 1 and 2, from Sphinx to capping Kc above western edge of Ankylosaur Flats. Includes same complex of sandslides and admixed fluvial deposits seen at Death Row.
Fig. 15 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 15. Schematic cross section of exposures on south side of Camel Humps Basin containing Camel Humps locality. Location is seen on maps 1 and 2.
Fig. 10 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 10. Exposures at Delta Force showing contact between vaguely cross-stratified sandstone of Facies E-2 (lower left), interpreted as eolian dune deposits, and structureless sandstone of Facies S (upper right), interpreted as dune-derived sandslide/debris flow deposits.
Fig. 8 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 8. Correlation chart of stratigraphic sections at Ukhaa Tolgod, including Zophia's Hill area (at far right). Sections are labeled and positions are plotted on maps 3–6. Lithologic key is included. Symbols such as 26°/98° represent the amount and azimuth of dip for cross-strata, which are inferred to represent the paleowind direction.
Fig. 7 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 7. Reddish brown siltstone of Facies M (especially to right of pack) exposed near the eastern base of Camel Humps, interpreted as interdune deposits formed in ephemeral lakes and ponds.
Fig. 20. A in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 20. A. Overview looking northeast at exposures of Zofia's Hill (right foreground) Zofia's Middle (center), and Zofia's North (left background). B. View looking east at Zofia's Middle with prominent bed of conglomerate (Facies C) exposed near the base (by crew members).
Fig. 4 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 4. Cross-stratified, tabular concretions of Facies E-2, exposed southwest of Xanadu, interpreted as early-cemented sheets that developed parallel to stratification within eolian dune deposits.
Fig. 5. A in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 5. A. Structureless sandstone with small lens of conglomerate of Facies S (below hammer), exposed at the base of the Sphinx, interpreted as sand slides down the lee slopes of eolian dunes (sandstone), mixed with fluvial gravel. B. Structureless sandstone with pebbles imbedded in matrix of Facies F interpreted as mass flow composed of a mixture of dune- and stream-derived material.
Fig. 12 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 12. Sphinx, showing low-relief exposures of structureless sandstone (Facies S) at the base and crossstratified sandstone (Facies E-1), which forms the butte.
Fig. 3 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 3. Cross-stratified sandstone of Facies E-1, exposed at Little Ukhaa, containing inverse-graded ripple laminations, interpreted as migration of eolian dunes (far right) and ripples (center and left).
Fig. 14 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 14. View looking east showing low ridge composed of siltstone (Facies M) below buttes of Camel Humps.
Fig. 2 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 2. Concave-up fold in cross-stratified sandstone of Facies E-1 interpreted as track of large vertebrate. Width of field of view is 30 cm.
Fig. 1 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 1. Cross-stratified sandstone of Facies E-1, exposed near the base of the Sphinx, interpreted as eolian dune deposits.
Fig. 9 in The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
Fig. 9. Top: Schematic cross section of exposures at Downlap Hill. Location of site is labeled on map 2. For lithologies in all cross sections, see fig. 8. Bottom: View looking north at Downlap Hill, with low-angle bedding in sandstone of Facies F (below person) underlying distinctly cross-stratified sandstone of Facies E- 1 (slightly above and to right of person). See top for interpretation.
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