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96 results for “dolomite”
3D geological models of dolomitized clinoforms and flow simulation results: scenario 2 in Teoh, C.P. et al (2021)
<p>3D geological models of dolomitized clinoforms (10 different realisations) and flow simulation results according to Scenario 2 in Teoh, C.P. et al (2021) doi:<a href="http://doi.org/10.1016/j.marpetgeo.2021.105344">10.1016/j.marpetgeo.2021.105344</a>.<br> Models are built using surface-based modelling approach (doi:<a href="https://doi.org/10.1007/s11004-018-9764-8">10.1007/s11004-018-9764-8</a>). Flow simulations are run with IC-FERST, using unstructured tetrahedral meshes that adapt to geological heterogeneity and flow behaviour throughout the simulation to improve simulation quality and performance.</p> <p>For each of the 10 stochastic realisations, 5 geological models are available with corresponding flow simulation results:<br> - Only clinoforms and facies boundaries<br> - 1 dolomite body per clinothem (~20% dolomite)<br> - 2 dolomite bodies per clinothem (~40% dolomite)<br> - 3 dolomite bodies per clinothem (~60% dolomite)<br> - 4 dolomite bodies per clinothem (~80% dolomite)<br> <br> Input model files for simulation are provided in Exodus (.e) and GMSH (.msh) formats.<br> Flow simulation settings are provided for IC-FERST in .mpml files (<a href="http://multifluids.github.io/">multifluids.github.io</a>)<br> Flow simulation results are provided as:</p> <ul> <li> 3D unstructured adaptive mesh in .vtu format, which can be opened with Paraview (www.paraview.org). Time interval between successive mesh outputs is 1 month.</li> <li> In- and outflow rates and volumetric proportions per phase in .csv</li> </ul> <p>Naming of files and folders:<br> <em>Sxxxxxx_yyyyz</em> where:<br> '<em>xxxxxx</em>' is the stochastic seed number used to sample the input statistics and create the geological model<br> '<em>yyyy</em>' is either 'clino' or 'dolo' to indicate if the model represents respectively only clinoforms, or contains dolomite bodies <br> '<em>z</em>' corresponds to the number of dolomite bodies per clinothem</p>
3D geological models of dolomitized clinoforms and flow simulation results: scenario 1 in Teoh, C.P. et al (2021)
<p>3D geological models of dolomitized clinoforms (10 different realisations) and flow simulation results according to Scenario 1 in Teoh, C.P. et al (2021) doi:<a href="http://doi.org/10.1016/j.marpetgeo.2021.105344">10.1016/j.marpetgeo.2021.105344</a>.<br> Models are built using surface-based modelling approach (doi:<a href="https://doi.org/10.1007/s11004-018-9764-8">10.1007/s11004-018-9764-8</a>). Flow simulations are run with IC-FERST, using unstructured tetrahedral meshes that adapt to geological heterogeneity and flow behaviour throughout the simulation to improve simulation quality and performance.</p> <p>For each of the 10 stochastic realisations, 5 geological models are available with corresponding flow simulation results:<br> - Only clinoforms and facies boundaries<br> - 1 dolomite body per clinothem (~20% dolomite)<br> - 2 dolomite bodies per clinothem (~40% dolomite)<br> - 3 dolomite bodies per clinothem (~60% dolomite)<br> - 4 dolomite bodies per clinothem (~80% dolomite)<br> <br> Input model files for simulation are provided in Exodus (.e) and GMSH (.msh) formats.<br> Flow simulation settings are provided for IC-FERST in .mpml files (<a href="http://multifluids.github.io/">multifluids.github.io</a>)<br> Flow simulation results are provided as:</p> <ul> <li> 3D unstructured adaptive mesh in .vtu format, which can be opened with Paraview (www.paraview.org). Time interval between successive mesh outputs is 1 month.</li> <li> In- and outflow rates and volumetric proportions per phase in .csv</li> </ul> <p>Naming of files and folders:<br> <em>Sxxxxxx_yyyyz</em> where:<br> '<em>xxxxxx</em>' is the stochastic seed number used to sample the input statistics and create the geological model<br> '<em>yyyy</em>' is either 'clino' or 'dolo' to indicate if the model represents respectively only clinoforms, or contains dolomite bodies <br> '<em>z</em>' corresponds to the number of dolomite bodies per clinothem</p>
Fig. 33 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 33. Rarefaction curves of Cassian assemblages from Misurina Landslide, Lago Antorno (assemblages studied herein), Settsass Scharte (Nützel and Kaim 2014) and Stuores Wiesen (Hausmann and Nützel 2015). Only bulk samples are used.
Fig. 28 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 28. Cardiid bivalve Septocardia pichleri (Bittner, 1895) from Lago Antorno, northern Italy, Cassian Formation, Carnian, Upper Triassic. PZO 12866, in ventral (A1), dorsal (A2), and lateral (A3, A4) views.
Fig. 24 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 24. Stuoraxid gastropod Ampezzogyra angulata Nützel and Hausmann sp. nov. from Lago Antorno (A, C) and Misurina Landslide (B, D), Cassian Formation, northern Italy, Late Triassic. A. Paratype PZO 12848, in oblique lateral (A1), apical (A2), and apertural (A3) views; A4, detail teleoconch at adapical whorl angulation with micro-ornament of fine tubercles; A5, protoconch in oblique lateral view; A6, protoconch in apical view; A7, crossed lamellar shell structure. B. Paratype PZO 12733, in oblique lateral (B1), apical (B2), and apertural (B3) views. C. Holotype PZO 12847, in apical (C1), basal (C2), and apertural (C3) views; C4, detail of C3; C5, detail teleoconch with micro-ornament of fine tubercles; C6, protoconch in apical view; C7, protoconch in oblique view. D. Paratype PZO 12734, in apical (D1) and apertural (D2) views.
Fig. 23. Hyalogyrinid gastropod Alexogyra marshalli Bandel, 1996 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 23. Hyalogyrinid gastropod Alexogyra marshalli Bandel, 1996 from Lago Antorno, northern Italy, Cassian Formation, Carnian, Upper Triassic. A. PZO 12842, in apical view. B. PZO 12843, in apertural view. C. PZO 12844, protoconch in oblique lateral view. D. PZO 12845, in oblique apertural view to show base.
Fig. 20 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 20. Mathildid gastropod Jurilda elongata (Leonardi and Fiscon, 1959) from Misurina Landslide, northern Italy, Cassian Formation, Carnian, Upper Triassic. A. PZO 12716, in lateral view (A1), A2, early whorls including heterostrophic protoconch, in lateral view. B. PZO 12717, in apical (B1) and lateral (B2) views; B3, early whorls including heterostrophic protoconch, in lateral view. C. PZO 12718, in apertural (C1) and oblique basal (C2) views. D. PZO 12719, in lateral (D1) and oblique basal (D2) views. E. PZO 12720, detail teleoconch whorl, in lateral view.
Fig. 16 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 16. Protorculid gastropods from Lago Antorno (A–D) and Misurina Landslide (E), northern Italy, Cassian Formation, Carnian, Upper Triassic. A. Atorcula sp., PZO 12816, in lateral view with drill holes (A1), A2, close up showing incomplete drill hole (right) and complete one (left). B. Atorcula sp., PZO 12817, in lateral view (B1), B2, close up showing drill hole. C. Atorcula canalifera (Münster, 1841), PZO 12819, in apertural view. D. Atorcula canalifera (Münster, 1841), PZO 12888, in apertural view. E. Atorcula canalifera (Münster, 1841), PZO 12697, axially ribbed larval shell and first smooth teleoconch whorls, in lateral view.
Fig. 13 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 13. Coelostylinid gastropods Helenostylina convexa (Nützel and Kaim, 2014) from Lago Antorno (A, B, C), Misurina Skilift (D), and Misurina Landslide (E), northern Italy, Cassian Formation, Carnian, Upper Triassic. A. PZO 12812, relatively large specimen with well-preserved base with spiral ribs, in apertural view (A1); A2, early whorls in lateral view; A3, basal view showing spiral ribs; A4, oblique basal view showing spiral ribs on base. B. PZO 12813, relatively large specimen with spiral ribs on base and protoconch with tubercles, in apertural view (B1); B2, close up of base showing spiral ribs on base; B3, early whorls with tubercles on larval shell, in lateral view. C. PZO 12814, juvenile shell with tubercles on larval shell, in lateral view. D. PZO 12694, juvenile shell with tubercles on larval shell and healed shell fracture, in apertural (D1) and lateral (D2, D4) views; details showing end of larval shell (arrows), in lateral (D3) and apical (D5) views. E. PZO 12695, relatively large specimen with well-preserved base with spiral ribs and protoconch with tubercles, in apertural view (E1); E2, oblique apertural view to show base with spiral ribs; E3, protoconch in lateral view.
Fig. 12 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 12. Caenogastropods from Lago Antorno (A) and Misurina Landslide (B–F), northern Italy, Cassian Formation, Carnian, Upper Triassic. A. Unidentified caenogastropod, PZO 12829, in lateral view. B. Coelostylina sp. 1, PZO 12691, in apertural view. C. Coelostylina sp. 2, PZO 12692, in lateral view. D. Flemingella bistriata (Münster, 1841), PZO 12713, in apertural view. E. Coelochrysalis pupaeformis (Münster, 1841), PZO 12714, in lateral view, with constriction of last whorl. F. Coelochrysalis pupaeformis (Münster, 1841), PZO 12715, deformed specimen in lateral view, showing constriction of last whorl.
Fig. 10 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 10. Coelostylinid gastropod Coelostylina conica (Münster, 1841) from Lago Antorno (A–D) and Misurina Landslide (E, F), northern Italy, Cassian Formation, Carnian, Late Triassic. A. PZO 12803, in apertural (A1) and abapertural (A2) views; A3, spire whorls in lateral view; A4, close up of spire whorl showing faint spirally arranged micro-pits; A5, close up of apical whorls in lateral view. B. PZO 12804 in apertural view. C. PZO 12805, with drill hole, in apertural view (C1); C2, early whorls including protoconch, in lateral view. D. PZO 12806, in lateral view (D1); D2, early whorls including protoconch, in lateral view; D3, whorl detail with boring. E. PZO 12686, in apertural view. F. PZO 12687, with drill hole in apertural view (F1); F2, detail, in apertural view.
Fig. 7 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 7. Naticopsid gastropod Hologyra? expansa (Laube, 1869), PZO 12802, from Lago Antorno, northern Italy, Cassian Formation, Carnian, Upper Triassic; apertural view showing callus on inner and parietal lip.
Fig. 6 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 6. Turbinid? gastropod "Turbo" sp., PZO 12740, from Misurina Landslide, northern Italy, Cassian Formation, Carnian, Upper Triassic. In apertural (A1) and lateral (A2), and apical (A3) views; A4, early whorls in lateral view.
Fig. 32 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 32. Trace fossils (taxonomic assignment unknown) from Misurina Landslide, northern Italy, Cassian Formation, Carnian, Upper Triassic. A. PZO 12822. B. PZO 12876. C. PZO 12877.
Fig. 5. Trochonematid gastropod Eunema badioticum Kittl, 1891, PZO 12796 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 5. Trochonematid gastropod Eunema badioticum Kittl, 1891, PZO 12796, from Lago Antorno, northern Italy, Cassian Formation, Carnian, Upper Triassic. In apertural (A1) and lateral (A2, A3) views; A4, detail of last whorl showing fine ornamentation including pits on upper angulation, in lateral view.
Fig. 17 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 17. Zygopleurid gastropods from Lago Antorno (A–C) and Misurina Landslide (D–H), northern Italy, Cassian Formation, Carnian, Upper Triassic. A. Ampezzopleura hybridopsis Nützel, 1998, PZO 12831, axially ribbed larval shell and 3 teleoconch whorls, in lateral view. B. Ampezzopleura hybridopsis Nützel, 1998, PZO 12832, axially ribbed larval shell and 1 teleoconch whorl, in lateral view (B1), B2, last whorl axial ribs reduced to subsutural nodes, in lateral view; B3, earliest whorls smooth, then strong axial ribs, in lateral view. C. Ampezzopleura hybridopsis Nützel, 1998, PZO 12833, axially ribbed larval shell. D. Ampezzopleura hybridopsis Nützel, 1998, PZO 12705, axially ribbed larval shell and 2 teleoconch whorls, in apertural (D1), lateral (D2), and apical D3) views. E. Ampezzopleura hybridopsis Nützel, 1998, PZO 12706, teleoconch. F. Ampezzopleurahybridopsis Nützel, 1998, PZO 12707, axially ribbed larval shell and 3 teleoconch whorls, in lateral view (F1), F2, protoconch in lateral view, axial ribs of larval shell reduced to subsutural nodes on last whorl; F3, protoconch in lateral view, axial ribs of larval shell reduced to subsutural nodes and teleoconch ribs begin to appaer on last whorl. G. Ampezzopleura hybridopsis Nützel, 1998, PZO 12708, axially ribbed larval shell and 4 teleoconch whorls, in lateral view. H. Ampezzopleura bandeli Nützel, 1998, PZO 12703, protoconch and ca. 4 teleoconch whorls.
Fig. 3 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 3. Rarefaction curves of surface and bulk samples from Misurina Landslide and Lago Antorno. A. Complete curves. B. Detailed view.
Fig. 1 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 1. Maps of northern Italy (A, B) showing the sampling localities Misurina Landslide and Lago Antorno (marked with stars). C. Upper part of Misurina Landslide locality where the samples were taken. D. Detailed view of the sediments at the Misurina Landslide locality.
Fig. 2 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 2. Species (A1, B1) and specimen (A2, B2) proportions within higher taxa of the bulk samples from Misurina Landslide (A) and Lago Antorno (B).
Fig. 27 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 27. Cassianellid bivalves from Lago Antorno, northern Italy, Cassian Formation, Carnian, Upper Triassic. A. Cassianella spp., PZO 12886, in lateral view (A1); A2, lateral view showing prodissoconch; A3, internal view with partly preserved hinge. B. Cassianella beyrichi Bittner, 1895, PZO 12861, in lateral view. C. Cassianella beyrichi Bittner, 1895, PZO 12862, in internal (C1) and lateral (C2) views.
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