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opencc-zeroJun 2024View details →

Dataset: Tectonic Therapeutic, Inc. (TECX) Stock Performance

This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.

opencc-zeroJun 2024View details →

Dataset: Tectonic Financial, Inc. (TECTP) Stock Performance

Fig. 9 in Stratigraphic And Tectonic Data On The Cretaceous Flysch In The Northern Ciuc Mountains (Eastern Carpathians, Romania)

Fig. 9 Geologic cross sections in the northern area of the Ciuc Mountains. The location of cross sections is marked on Fig. 1.

Fig. 5 in Stratigraphic And Tectonic Data On The Cretaceous Flysch In The Northern Ciuc Mountains (Eastern Carpathians, Romania)

Fig. 5 Diagram of the lithologic types in the Bistra Sandstone (= Ugra Sandstone) showing binary depositional rhythms, as occurring in the Jandarmului and Ugra valleys.

Fig. 2 in Stratigraphic And Tectonic Data On The Cretaceous Flysch In The Northern Ciuc Mountains (Eastern Carpathians, Romania)

Fig. 2 Stratigraphic column of the Cretaceous flysch in the Ciuc Digitation of the Ceahlău Nappe, between the TrotuȘ River and Șulța Streamlet. Legend: 1, marl; 2, marly limestone; 3, sandy limestone; 4, calcarenite; 5, sandstone; 6, marly clay; 7, calcareous breccia; 8, macrofossil occurrence.

Fig. 12 in Stratigraphic And Tectonic Data On The Cretaceous Flysch In The Northern Ciuc Mountains (Eastern Carpathians, Romania)

Fig. 12 Peregrinella multicarinata (Lamarck, 1819) [= peregrina von Buch, 1835], Ciugheş Valley, Cădăreşti; 1 well-preserved specimen (LPBIII 376) in 1a – ventral; 1b – lateral; 1c - dorsal views; 2 rock slab with broken shells (LPBIII 376); scale bars represent 2 cm.

Fig. 11 in Stratigraphic And Tectonic Data On The Cretaceous Flysch In The Northern Ciuc Mountains (Eastern Carpathians, Romania)

Fig. 11 Geologic cross sections in the GhimeȘ-Palanca region: A – Cross section at the GhimeȘ Pass, at the confluence of the Șanț Streamlet with the TrotuȘ River. B – Cross section at the Palanca Railway Station, at the confluence of the CiugheȘ Valley with the TrotuȘ River; Legend: 1, coarse-grained micaceous sandstone; 2, convolute calcareous fine-grained sandstone; 3, sideritic fine-grained sandstone; 4, red clay with pelosiderites; 5, marly clay; 6, convolute micaceous sandstone; 7, rusty marly limestone.

opencc-by-4.0Aug 2024View details →

Recent Tectonic Activity in and Around the Posidonius Crater, Moon-Version 5

The shapefiles and .scc files of the version 5 manuscript: "Recent tectonic activity in and around the Posidonius crater, Moon."

opencc-by-4.0Dec 2020View details →

Extending full-plate tectonic models into deep time: Linking the Neoproterozoic and the Phanerozoic

This file describes the plate model accompanying Merdith et al. (in review), 'A continuous, kinematic full-plate motion model from 1 Ga to present'.  It is a compilation of four plate models: Domeier (2016; 2018); Merdith et al. (2017); Young et al. (2019) and presented purely in a palaeomagnetic reference frame derived from Tetley (2018). This directory contains Merdith_etal_2021_ESR_v1.2.4.gproj, which is a GPlates project file that will load the following: 1000_0_rotfile_Merdith_etal.rot - the Global Rotation Model but with a purely paleomagnetic reference frame 1000_410-*{Convergence/Divergence/Transform/Topologies}-Merdith_etal.gpml - the plate topologies for 1000 to 410 Ma 410-250_plate_bounds_Merdith_etal.gpml - the plate topologies for 410 to 250 Ma 250-0_plate_bounds_Merdith_etal.gpml - the plate topologies for 250 to 0 Ma TopologyBuildingBlocks_Merdith_etal.gpml - building blocks for some topologies between 410 and 0 Ma coastlines_Merdith_etal.gpml - a Global Coastline file (mainly for the past 400 Ma) continents_Merdith_etal.gpml - a Global Continent shapes file (for the past 1 Ga) cratons_Merdith_etal.gpml - a Global cratonic shapes file (for the past 1 Ga) static_polygons_Merdith_etal.gpml - a Global static polygon file (for the past 1 Ga) 1000-410_poles.gpml - collection of palaeomagnetic data used to constrain the model between 1000 and 410 Ma (corresponds to Table 1 in the associated publication) For the Mesozoic and Cenozoic, the plates comprising the Pacific Ocean traditionally move in a separate reference to the other ocean basins and continental motions, instead defined by hotspot motion. In order to preserve the plate motion of the Pacific relative to the continental domains where the new GAPWAP was implemented, we extracted relative plate rotations between the Pacific (plateID: 901) and Africa (plateID: 701) in 5 Ma intervals between 250 and 83 Ma from the Young et al. (2019) model, which has been corrected for errata as discussed in Torsvik et al. (2019). This results in the same relative motion of all Pacific plates to continental plates; however it slightly alters the absolute position of the Pacific plates between 250 and 83 Ma. Studies interested in short(er) timescale (< 5 Ma) analysis or absolute plate motions should use a different model that explicitly links plate motion with the mantle (e.g. (Muller et al. 2019; Tetley et al. 2019)). To be clear, if you want to analyse the Pacific Ocean, including hotspot motion, Hawaiian-Emperor Bend kinematics etc. you should not use this model. To load these datasets in GPlates do the following: 1.  Open GPlates 2.  Pull down the GPlates File menu and select Open Project 3.  Click to select the GPROJ file 4.  Click Open Alternatively, drag and drop the GPROJ file onto the globe. You now have a global present day continents loaded in GPlates as well as the underlying rotation model and evolving plate topologies.  Play around with the GPlates buttons to make an animation, select features, draw features, etc. For more information, read the GPlates manual which can be downloaded from <a href="https://www.gplates.org">www.gplates.org.</a>  The agegrids associated with this model were subsquently developed as part of the <a href="../records/10910449" target="_blank" rel="noopener">Muller et al. 2022</a> model and can be accessed at: <a href="https://repo.gplates.org/webdav/PlateModel_Age_SR_Grids/Muller_etal_2022_SE/" target="_blank" rel="noopener">https://repo.gplates.org/webdav/PlateModel_Age_SR_Grids/Muller_etal_2022_SE/</a>.

opencc-by-4.0Jul 2022View details →

A tectonic-rules-based mantle reference frame since 1 billion years ago – implications for supercontinent cycles and plate–mantle system evolution

The archive Muller_etal_2022_SE_1Ga_Opt_PlateMotionModel.zip contains the files for the plate model in an optimised mantle reference frame. GPlates or pyGPlates software (<a href="https://www.gplates.org/">www.gplates.org</a>) is needed to read these files.  The archive Muller_etal_2022_SE_mantle-ref-frame-oceanic-crustal-agegrids.zip contains the oceanic crustal age grids in netCDF-4 format for the optimised mantle reference frame plate model, while the archive Muller_etal_2022_SE_PMAG_oceanic-crustal-agegrids.zip contains the oceanic crustal age grids in netCDF-4 format for the paleomagnetic reference frame plate model from Merdith et al. (2021).   The agegrids associated with this model can be accessed at: <a href="https://repo.gplates.org/webdav/PlateModel_Age_SR_Grids/Muller_etal_2022_SE/" target="_blank" rel="noopener">https://repo.gplates.org/webdav/PlateModel_Age_SR_Grids/Muller_etal_2022_SE/</a>

Fig. 19 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism

Fig. 19. Right mandible (UNSM 44813) and maxilla (UNSM 44814) of the oreodont Merycochoerus magnus from the Carpenter Ranch Formation, Merycochoerus Butte, Goshen County, Wyoming.

Fig. 16 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism

Fig. 16. Diaphysis of chalicothere limb bone (UNSM 44825) showing greenbone fracturing produced by scavengers, with broken margins overprinted by preburial abrasion, East Sturdivant Butte, Cow Trail Notch local fauna, Carpenter Ranch Formation, Sioux County, Nebraska. Note marrow cavity packed with granitic gravel.

Fig. 12 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism

Fig. 12. Cranial dome of the chalicothere Tylocephalonyx (UNSM 44801), external surface of the dome, Carpenter Ranch Formation, Deahl Butte, Goshen County, Wyoming (presumed anterior face to left, dorsal upward).

Fig. 6 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism

Fig. 6. Type area of the Carpenter Ranch Formation, early Miocene, WyomingNebraska: (A) Cow Trail Notch stratotype section (at arrow) in NW1/4, SW1/4, NE1/4, SW1/4, sec. 36, T27N, R58W, Sioux County, Nebraska, looking northeast toward the west escarpment of East Sturdivant Butte within Sturdivant Gap. The Cow Trail Notch fauna was collected entirely from the promontory where the section was measured. The high surface of East Sturdivant Butte is mantled by a thin lag deposit of Oberg gravel not to be confused with the indurated Carpenter Ranch Formation gravel in the type section and contiguous outcrops in the gap. Sheep Creek runs in the foreground. (B) East escarpment of West Sturdivant Butte in Sturdivant Gap, looking west, immediately opposite figure 6A, showing the cliffforming Carpenter Ranch Formation caprock overlying finegrained Arikaree and White River strata. Truck on access road through the gap is situated at the WyomingNebraska state boundary.

Fig. 15. Proximal metacarpal 4 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism

Fig. 15. Proximal metacarpal 4 (UNSM 44804) referred to (?)Tylocephalonyx, Carpenter Ranch Formation, Goshen County, Wyoming: A, radial face showing the dorsal (d) and volar (v) facets for metacarpal 3; B, proximal articular surface for the unciform (u). Stereopairs. Finest divisions of scale in mm.

Fig. 7 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism

Fig. 7. Stratotype section of the Carpenter Ranch Formation (fig. 6A), west escarpment of East Sturdivant Butte, Sioux County, Nebraska, which includes the Cow Trail Notch local fauna. Early Hemingfordian mammals of the Cow Trail Notch local fauna include the dromomerycid Aletomeryx, moschid Pseudoblastomeryx, and canid Phlaocyon. Lithic symbols as in fig. 9.

Fig. 9 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism

Fig. 9. Measured section of the Carpenter Ranch Formation at Deahl Butte at the locality yielding the partial cranial dome (UNSM 44801) and mandible (UNSM 44800) of the chalicothere Tylocephalonyx (table 3). The dome, mandible, and diaphysis of a femur (UNSM 44802) were found in proximity within a crystalline gravel lens. Here Arikaree gray sands intervene between the incised Carpenter Ranch paleovalley and Brule Formation. Lithic symbols apply to figures 7–9.

Fig. 5 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism

Fig. 5. Redrafted version of N.H. Darton's crosssection (1899: fig. 213) from Spoon Butte to Sturdivant's Ranch, showing the silicacemented sandstone caprocks descending in elevation to the south. Darton regarded all the caprocks as ''Arikaree'' conglomerates, ''consisting in large part of crystalline rocks and apparently lying on a steeply sloping surface''. The letters AE were not explained in his caption. Note correspondence to figure 3.

Fig. 4 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism

Fig. 4. Principal fossil mammal localities (indicated by arrows) in the capping sandstones of the Patrick Buttes. Cow Trail Notch at East Sturdivant Butte and sites at Merycochoerus Butte have yielded most of the agediagnostic specimens in the early Hemingfordian Carpenter Ranch Formation. Deahl Butte produced the partial dome and mandible of the chalicothere (UNSM 44800, 44801). Barstovian sites in the Spoon Butte Beds include South Rim, GF Butte, North Point and Box Canyon. The Oberg Quarries are gravel pits containing waterworn mid and late Miocene mammals and Pleistocene Equus.

Fig. 1 in An Early Miocene Dome-Skulled Chalicothere from the ''Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism

Fig. 1. Geographic map of the Patrick Buttes, WyomingNebraska. The areal extent of each butte is indicated by solid and/or dashed lines marking the limits of the butte caprocks, formed by silicacemented sandstone. Names for individual buttes are derived from historical usage, local practice, and UNSM field terms.