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6 results for “gneiss”
Mechanical and hydraulic transport properties of transverse-isotropic Gneiss deformed under deep reservoir stress and pressure conditions.
<p>"This is the ReadMe file corresponding to the study entitled: "Mechanical and hydraulic transport properties of transverse-isotropic<br> Gneiss deformed under deep reservoir stress and pressure conditions" <br> <br> "By M. Acosta, & M. Violay." <br> <br> This study has been published in the International Journal of Rock Mechanics and Mining Sciences in June 2020. <br> https://doi.org/10.1016/j.ijrmms.2020.104235<br> <br> This Read-Me file has been last edited on 2020-06-31 <br> <br> This readme file describes the data repository and supplementary files accompanying the above publication. <br> For any further queries please contact mateo.acosta@epfl.ch <br> <br> The following files are included: <br> <br> --- Regarding Figure 3. <br> <br> "1) ""Acosta_et_al_2020_Figure3Data.xlsx"" " <br> This is the processed data from the experiments described in Figure1 of the article. <br> "In this .xlsx File, each sheet corresponds to one figure panel as follows: " <br> <br> Fig.3: One experiment example<br> Column A: Axial strain in (%) ; Column B: Effective axial stress (in MPa); Column C: Axial strain for AE's in (%) ; Column D: Acoustic emission hits (in #); Column D: Axial strain for porosity change in (%) ; Column E: Porosity change (in %);</p> <p>--- Regarding Figure 4. <br> <br> "1) ""Acosta_et_al_2020_Figure4Data.xlsx"" " <br> This is the processed data from the experiments described in Figure1 of the article. <br> "In this .xlsx File, each sheet corresponds to one figure panel as follows: " <br> <br> Fig.4a&g: Beta=0deg<br> Column A: Axial strain in (%) ; Column B: Effective axial stress (in MPa); Column C: Axial strain for AE's in (%) ; Column D: Acoustic emission hits (in #); Column D: Axial strain for porosity change in (%) ; Column E: Porosity change (in %);</p> <p>Fig.4b&h: Beta=30deg<br> Column A: Axial strain in (%) ; Column B: Effective axial stress (in MPa); Column C: Axial strain for AE's in (%) ; Column D: Acoustic emission hits (in #); Column D: Axial strain for porosity change in (%) ; Column E: Porosity change (in %);</p> <p>Fig.4c&i: Beta=45deg<br> Column A: Axial strain in (%) ; Column B: Effective axial stress (in MPa); Column C: Axial strain for AE's in (%) ; Column D: Acoustic emission hits (in #); Column D: Axial strain for porosity change in (%) ; Column E: Porosity change (in %);</p> <p>Fig.4d&j: Beta=60deg<br> Column A: Axial strain in (%) ; Column B: Effective axial stress (in MPa); Column C: Axial strain for AE's in (%) ; Column D: Acoustic emission hits (in #); Column D: Axial strain for porosity change in (%) ; Column E: Porosity change (in %);</p> <p>Fig.4e&k: Beta=90deg<br> Column A: Axial strain in (%) ; Column B: Effective axial stress (in MPa); Column C: Axial strain for AE's in (%) ; Column D: Acoustic emission hits (in #); Column D: Axial strain for porosity change in (%) ; Column E: Porosity change (in %);</p> <p>Fig.4f&l: LPG<br> Column A: Axial strain in (%) ; Column B: Effective axial stress (in MPa); Column C: Axial strain for AE's in (%) ; Column D: Acoustic emission hits (in #); Column D: Axial strain for porosity change in (%) ; Column E: Porosity change (in %);</p> <p>--- Regarding all other Figures, the tables provided in the article allow reproduction of these.</p> <p> </p>
Fluid-driven mass transfer during retrograde metamorphism and exhumation of the UHP Western Gneiss Region terrane, Norway
<p>This dataset contains supplementary files for the published manuscript entitled "Fluid-driven mass transfer during retrograde metamorphism and exhumation of the UHP Western Gneiss Region terrane, Norway."</p>
The composite metamorphic sequence in the Jiajika gneiss dome, Songpan-Ganze orogenic belt, eastern Tibet: P–T–D–t evolution and implications for lithium mineralization
<p>This is the dataset for "The composite metamorphic sequence in the Jiajika gneiss dome, Songpan-Ganze orogenic belt, eastern Tibet: P–T–D–t evolution and implications for lithium mineralization". The dataset includes EMPA, whole-rock major elements, and geochronological data.</p>
Gneiss dome exhumation aided by extrusion along a step-form detachment in the Eastern Pamir
<p>Supplementary data for submission "Gneiss dome exhumation aided by extrusion along a step-form detachment in the Eastern Pamir" to G-cubed. </p>
An East Africa origin for Madagascar: evidence from zircon U-Pb geochronology and geochemistry of Neoarchean gneisses and granitoids from the Maevatanana greenstone belt in Madagascar
<p><strong>Table 1 </strong>Results of zircon U–Pb dating of sample G1 from the melanosome bands in the gneiss</p> <p><strong>Table 2 </strong>Results of zircon U–Pb dating of sample M33 from the Neoarchean granitoids</p> <p><strong>Table 3 </strong>Zircon Hf isotopic data for the melanosome bands in the gneiss</p> <p><strong>Table 4 </strong>Zircon Hf isotopic data for Neoarchean granitoids</p> <p><strong>Table 5 </strong>Major element (wt%), trace element (ppm), and REE (ppm) composition of the melanosome bands in the gneiss</p> <p><strong>Table 6 </strong>Major element (wt%), trace element (ppm), and REE (ppm) composition of the Neoarchean granitoids</p>
Text-fig. 1. Geological map of the site Kučlín, Trupelník Hill. 1 – dumpsite body, exploitation faces, 2 – landslide body, 3 – occurrence of the basalt in the landslide body, 4 – tuff, tuffite with gneiss particles, 5 – 11 – Late Eocene rocks. 5 – basalts, 6 – tuff, tufite, 7 – diatomaceous cherts layer enclosing lenses of diatomaceous earth, 8 – diatomitic breccia, 9 – diatomaceous shale, 10 – diatomaceous clays to diatomites, 11 – calcareous diatomaceous clays to diatomaceous limestones and re-deposited Cretaceous material, 12 – Late Turonian marlstone to limestone, 13 – Middle Turonian marlstone, 14 – Middle Turonian organo-detritic limestone to conglomerate, 15 – Late Proterozoic orthogneiss, 16 – Syčivka creek, 17 – road, field drives, 18 – Kučlín village. in Geology Of The Site Kučlín, Trupelník Hill Near Bílina In North Bohemia
Text-fig. 1. Geological map of the site Kučlín, Trupelník Hill. 1 – dumpsite body, exploitation faces, 2 – landslide body, 3 – occurrence of the basalt in the landslide body, 4 – tuff, tuffite with gneiss particles, 5 – 11 – Late Eocene rocks. 5 – basalts, 6 – tuff, tufite, 7 – diatomaceous cherts layer enclosing lenses of diatomaceous earth, 8 – diatomitic breccia, 9 – diatomaceous shale, 10 – diatomaceous clays to diatomites, 11 – calcareous diatomaceous clays to diatomaceous limestones and re-deposited Cretaceous material, 12 – Late Turonian marlstone to limestone, 13 – Middle Turonian marlstone, 14 – Middle Turonian organo-detritic limestone to conglomerate, 15 – Late Proterozoic orthogneiss, 16 – Syčivka creek, 17 – road, field drives, 18 – Kučlín village.
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