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8 results for “Evaporites”
Text-fig. 4. Type specimens of Magnolia allasoniae MARTINETTO sp. nov. from the Pliocene locality Ca' Viettone. a1–a4: Holotype (MGPT-PU141081) in different views, i.e., as originally figured in Martinetto (1995: pl. 1, fig. 5) in a black and white print (a1), in a new digital photograph in basal view (a2), ventral view (a3) and dorsal view (a4); b1–b4: Paratype MGPT-PU141082 in different views, i.e., as originally figured in Martinetto (1995: pl. 1, fig. 4) in a black and white print (b1), in a new digital photograph in basal view (b2), ventral view (b3) and dorsal view (b4); c1–c4: Paratype MGPT-PU141083 in different views, i.e., as originally figured in Martinetto (1995: pl. 1, fig. 6) in a black and white print (c1), in a new digital photograph in basal view (c2), ventral view (c3) and dorsal view (c4); d1–d4: Paratype MGPT-PU141084 in different views, i.e., as originally figured in Martinetto (1995: pl. 1, fig. 7) in a black and white print (d1), in a new digital photograph in basal view (d2), ventral view (d3) and internal view (d4). Scale bars 1 mm. in Late Messinian Flora From The Post-Evaporitic Deposits Of The Piedmont Basin (Northwest Italy)
Text-fig. 4. Type specimens of Magnolia allasoniae MARTINETTO sp. nov. from the Pliocene locality Ca' Viettone. a1–a4: Holotype (MGPT-PU141081) in different views, i.e., as originally figured in Martinetto (1995: pl. 1, fig. 5) in a black and white print (a1), in a new digital photograph in basal view (a2), ventral view (a3) and dorsal view (a4); b1–b4: Paratype MGPT-PU141082 in different views, i.e., as originally figured in Martinetto (1995: pl. 1, fig. 4) in a black and white print (b1), in a new digital photograph in basal view (b2), ventral view (b3) and dorsal view (b4); c1–c4: Paratype MGPT-PU141083 in different views, i.e., as originally figured in Martinetto (1995: pl. 1, fig. 6) in a black and white print (c1), in a new digital photograph in basal view (c2), ventral view (c3) and dorsal view (c4); d1–d4: Paratype MGPT-PU141084 in different views, i.e., as originally figured in Martinetto (1995: pl. 1, fig. 7) in a black and white print (d1), in a new digital photograph in basal view (d2), ventral view (d3) and internal view (d4). Scale bars 1 mm.
Text-fig. 3. Examples of plant macrofossil assemblages from post-evaporitic sections. a: bedding plane from Ciabòt Cagna covered by impressions of plant parts, with dominance of leaves of cf. Oleinites liguricus M.SACHSE, MCEA-P05038. b: waterloggedcompressed seeds of Toddalia latisiliquata (R.LUDW.) H.-J.GREGOR sieved out of a bulk sediment sample from Pollenzo, MGPTPU141033. c: millimeter-sized, waterlogged-compressed seeds of Sambucus pulchella C.REID et E.REID with abundant cracks, probably formed during both diagenesis and extraction of the fossils (bulk sediment sample from Ciabòt Cagna), MGPT- in Late Messinian Flora From The Post-Evaporitic Deposits Of The Piedmont Basin (Northwest Italy)
Text-fig. 3. Examples of plant macrofossil assemblages from post-evaporitic sections. a: bedding plane from Ciabòt Cagna covered by impressions of plant parts, with dominance of leaves of cf. Oleinites liguricus M.SACHSE, MCEA-P05038. b: waterloggedcompressed seeds of Toddalia latisiliquata (R.LUDW.) H.-J.GREGOR sieved out of a bulk sediment sample from Pollenzo, MGPTPU141033. c: millimeter-sized, waterlogged-compressed seeds of Sambucus pulchella C.REID et E.REID with abundant cracks, probably formed during both diagenesis and extraction of the fossils (bulk sediment sample from Ciabòt Cagna), MGPT-
Text-fig. 2. Stratigraphic columns of Govone (1), Sioneri (2), Ciabòt Cagna (3) and Pollenzo (4) sections. in Late Messinian Flora From The Post-Evaporitic Deposits Of The Piedmont Basin (Northwest Italy)
Text-fig. 2. Stratigraphic columns of Govone (1), Sioneri (2), Ciabòt Cagna (3) and Pollenzo (4) sections.
Text-fig. 1. Geographical location of the studied post-evaporitic sections (Piedmont Basin): Govone (1), Sioneri (2), Ciabòt Cagna (3) and Pollenzo (4). in Late Messinian Flora From The Post-Evaporitic Deposits Of The Piedmont Basin (Northwest Italy)
Text-fig. 1. Geographical location of the studied post-evaporitic sections (Piedmont Basin): Govone (1), Sioneri (2), Ciabòt Cagna (3) and Pollenzo (4).
Text-fig. 1. Context and location of the Govone outcrop. a: Location of the Piedmont Basin at the northern margin of the Mediterranean Basin and distribution of Messinian evaporites. b: Simplified geological map of the Piedmont Basin showing the location of the Govone outcrop close to the town of Alba. in Remains Of A Subtropical Humid Forest In A Messinian Evaporitebearing Succession At Govone, Northwestern Italy - Preliminary Results
Text-fig. 1. Context and location of the Govone outcrop. a: Location of the Piedmont Basin at the northern margin of the Mediterranean Basin and distribution of Messinian evaporites. b: Simplified geological map of the Piedmont Basin showing the location of the Govone outcrop close to the town of Alba.
(Magnetic dataset) High-Resolution Magnetic Investigation of a Hydrothermal System in a Volcanic-Evaporitic Environment
<p>This is the ground magnetic dataset collected in hydrothermal vent field sites (called Yellow Lake Fissure and the surrounding area near Dallol Dome) in the Danakil Depression, Ethiopia.</p> <p>The dataset consists of 12 profiles and 2 grided data. and useful geological locations.</p> <p>The dataset is in Excel spreadsheet format and consists of 15 sheets (12 profiles, 2 grid data and other useful points).</p> <p>The format of each profile and grid consists of 8 columns and is formatted as below</p> <p>Latitude(dd°mm.mmmm'), Longitude(ddd°mm.mmmm'), Altitude(meter), Date(yyyy-mm-dd), UTC_time(hhmmss), MagneticField(nT), MagneticAnomaly(nT), Signal_Quality</p> <p> </p>
McMurdo Dry Valleys Mineralogic composition of cryogenic evaporites determined by low-temperature X-ray diffactometry
As part of a collaborative investigation between researchers at Rice University, Arkansas State University, University of Rochester, and Ohio State University, lakes of the McMurdo Dry Valleys were sampled at discreet depth intervals during the 2005-2006 field season.  Sample splits were subsequently analyzed for chemical and isotopic composition of both gases and dissolved  ions, as well as dissolved organic carbon. In addition, cryogenic salts were sampled in the surrounding lake shores in order to determine the salt sources. Gravity cores were also obtained and in the case of Lake Vanda, a white precipitate was recovered from the lake bottom.        Presented  in this file is the mineralogic composition of salt crusts that were collected on the surface of sediment and rocks surrounding the lakes, as well as the lake-bottom precipitate from Lake Vanda.  The results are based on low-temperature XRD determinations, and Rietveld refinement of whole peaks.       Â
Rapid Karstification Process with Evaporite-Driven Sinkholes in Southern Kohat Basin, NW Pakistan
<p>This file consists of datasets (GIS files, InSAR Velocities, Electrical resistivity data, and profiles) used in our study. </p>
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