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10 results for “facies analysis”
FIG. 3 in Foraminiferal biostratigraphy, facies and sequence stratigraphy analysis across the K-Pg Boundary in Hazara, Lesser Himalayas (Dhudial Section)
FIG. 3. — Lithostratigraphic column showing the lithology, constituents and facies of the Dhudial Section.
FIG. 5 in Foraminiferal biostratigraphy, facies and sequence stratigraphy analysis across the K-Pg Boundary in Hazara, Lesser Himalayas (Dhudial Section)
FIG. 5. — Photomicrographs of thin slides: A, Planktonic foraminifera () and ferroan euhedral dolomite crystals () (S# 09); B, dolomitized zone () with planktonic foraminifera (), radiolarians () and ostracods () (S# 25); C, contact of the foraminiferal wackestone and packstone patch (S# 22); D, radiolarian rich facies showing radiolarians () and calcispheres () (S# 18); E, Heterohelix sp. () along with radiolarians () and ostracods () (S# 17); F, dolomitized zone between the lime mudstone (MS) and wackestone (WS) (S# 11); G, tectonic induced fracturing (S# 07); H, radiolarians () and zoned ferroan dolomite crystals in the mudstone facies (S# 11); I, well rounded feldspar grains (S# 38); J, chert lithic (S# 36); K, ferruginous matrix (S# 37); L, quartz () and feldspar () grains in Hangu Formation (S# 38). Scale bars: A-C, F, G, 200 µm; D, E, H-L, 100 µm.
FIG. 1 in Foraminiferal biostratigraphy, facies and sequence stratigraphy analysis across the K-Pg Boundary in Hazara, Lesser Himalayas (Dhudial Section)
FIG. 1. — Regional geological map after Burg (2011). The red square corresponds to studied location at Dhudial.
FIG. 9 in Foraminiferal biostratigraphy, facies and sequence stratigraphy analysis across the K-Pg Boundary in Hazara, Lesser Himalayas (Dhudial Section)
FIG. 9. — Sketch showing the platform evolution through different stages. The platform geometry in the early Campanian time (Stage I) during deposition of Kawagarh Formation was characterized by a steeper ramp. An incised valley and sequence boundary developed in Stage II during Selandian and the platform configuration became much gentler during the Thanetian (Stage III) as the accommodation space filled up.
FIG. 7 in Foraminiferal biostratigraphy, facies and sequence stratigraphy analysis across the K-Pg Boundary in Hazara, Lesser Himalayas (Dhudial Section)
FIG. 7. — Chart showing the sequence stratigraphic framework, sea level changes and paleoecology of the Dhudial Section.
FIG. 8 in Foraminiferal biostratigraphy, facies and sequence stratigraphy analysis across the K-Pg Boundary in Hazara, Lesser Himalayas (Dhudial Section)
FIG. 8. — Chart showing the planktonic foraminiferal distribution and biozones of the Dhudial Section.
Fig. 17 Carbonate facies from the breccia levels. a-d in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 17 Carbonate facies from the breccia levels. a-d Peloidal-bioclastic packstone with cyanobacteria, ostracods and foraminifera (d); cavities are filled with vadose silt and gravitational terrigenous material. e-f Breccia with horizontal (e), circumgranular and vertical (f) cracks. Scale-bar = 1 mm.
FIG. 2 in Foraminiferal biostratigraphy, facies and sequence stratigraphy analysis across the K-Pg Boundary in Hazara, Lesser Himalayas (Dhudial Section)
FIG. 2. — Generalized stratigraphy of the study area (Shah 2009).
FIG. 4 in Foraminiferal biostratigraphy, facies and sequence stratigraphy analysis across the K-Pg Boundary in Hazara, Lesser Himalayas (Dhudial Section)
FIG. 4. — Field photograph of the studied Dhudial Section: A, stratigraphic contacts of different ages; B, authigenic quartz near the boundary; C, Outcrop view of probable OAE3.
Fig. 2 Reefal facies. a-c in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 2 Reefal facies. a-c Coral-microbial boundstone; coral colonies are heavily encrusted by problematic microorganisms (a) or bordered by syndepositional, radiaxial-fibrous cements (b). d-h Bioclastic packstone (d, e, g-h) and bioclastic grainstone (f) internal sediment with dasycladalean algae [Steinmanniporella kapelensis (Sokač & Nikler)] (d), sponges (e), mollusks, corals, Crescentiella (f), microstalactitic (g) and microthrombolitic (h) microbial crusts.
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OpenNeuro
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