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40 results for “Makran”
Data from: Dating and morpho-stratigraphy of uplifted marine terraces in the Makran subduction zone (Iran)
<p>This data comes from the study of marine terraces from the Iranian Makran. This second version contains .zip compressed files instead of .rar .<br> A_files are seven terrace maps of the region of Jask, Tang, Gurdim, Konarak, Chabahar-Ramin, Lipar and Pasabander.<br> B_file are results of Radiocarbon and 230Th/U dating of mollusk shells from the marine deposits above the terraces.<br> C_file are results of Optically Stimulated Luminescence dating (OSL) of said deposits.<br> D_files are field pictures.<br> The data is published in support for the paper mentioned in the title (submitted to Earth Surface Dynamics).</p> <p>Brief description:<br> Terrace maps are accompanied with a datamodel excel file explaining the different GIS layers.<br> The maps are provided in both .KMZ files (for Google Earth) and Shapefiles</p> <p>Radiometric (i.e. both Radiocarbon and 230Th/U) analytical details are provided, together with XRD analysis of the Aragonitic shells and some SEM pictures of both Aragonitic and Calcitic shells. Method details are in the paper.</p> <p>OSL results are provided with the analytical details, such as: Environmental dose parameters, OSL raw measurements (out of the machine), OSL Histograms, Dose-Recovery tests and Fading test results. Method details are in the paper.</p> <p>Additional field pictures are provided with their legends (.txt file) and geolocalisation (.kmz file).</p>
Data for: Extention at the coast of the Makran subduction zone (Iran)
<p>This dataset comes from the study of normal faults at the coast of the Iranian Makran, near the city of Chabahar. The data is published in support for the paper mentioned in the title.</p> <p>The dataset contains:<br> A - A series of fault measurements made in the region of Chabahar, with the following subgroups:<br> a) Major Faults of Chabahar headland, b) minor faults of Chabahar headland, c) faults measured from the Konarak headland, d) faults measured in the Parak area, in the Makran ranges north of Chabahar, e) Bedrock bedding orientations.</p> <p>B - Shapefiles and KMZ file containing the structural measurements in A.</p> <p>C - Field pictures of normal faults and observed evidence of overpressure in Tertiary sediments.</p>
Data for: Pleistocene coastal evolution of the Makran subduction zone
<p>This dataset contain a set of field pictures made along the coast of the western Makran subduction zone, near the region of Chabahar.<br> A youtube video (diaporama) presents (some of) these figures in their context. <a href="https://www.youtube.com/watch?v=VRxXaCPRoJk&t=1s">https://www.youtube.com/watch?v=VRxXaCPRoJk&t=1s</a></p> <p>The field pictures are a visual support for the publication mentioned in the title.</p> <p>The dataset comes in the form of many field pictures classified in themes, their legends in text files and geolocalisation in a .kmz file.<br> BB and HB are bay beach and headland beach pictures, respectively<br> Pictures of the different marine terraces areas visited are labelled as follow:<br> CH - Chabahar marine terraces<br> GU - Gurdim marine terrace<br> JA - Jask marine terrace<br> KO - Konarak marine terraces<br> LI - Lipar marine terraces<br> PA - Pasabander marine terraces<br> RA - Ramin marine terraces<br> TA - Tang marine terraces</p> <p>M pictures are from tertiary marl bedrock outcrops along the coast</p> <p>Pictures B, C, D, E, F, G, and I are from major normal faults at Chabahar headland. A figure shows their localisation.</p> <p>Finally, many pictures illustrate the different sedimentary sections described and studied in the paper.</p>
Data for: Holocene sedimentary record and coastal evolution in the Makran subduction zone (Iran)
<p>The data comes from the study of Holocene beaches from the Iranian Makran. More exactly, the beaches in Pozm bay, Chabahar bay and the longitudinal beach west of the village of Beris. The data contain field pictures and their legends, results and analytical details of radiocarbon dating, SEM secondary electron images of the analysed shells and the results and analytical details of optically stimulated luminescence dating (OSL).<br> The data is published in support for the paper mentioned in the title.</p> <p>A to D are field pictures and legends of:<br> A - Pozm bay field pictures<br> B - Chabahar bay field pictures<br> C - Beris beach field pictures<br> D - Observed current depositional settings</p> <p>E - Radiocarbon dating results and analytical supplementary information<br> F - Secondary electrons SEM images of the analysed shells</p> <p>G - OSL dating results and analytical supplementary information</p> <p>Radiocarbon analytical details are provided, together with XRD analysis of the Aragonitic shells, SEM secondary electron images of analysed shells and calibration details. Method details are in the paper.</p> <p>OSL results are provided with the analytical details, such as: Environmental dose parameters, OSL raw measurements (out of the machine), OSL Histograms and Dose-Recovery tests. Method details are in the paper.</p>
Mechanism of the 2017 Mw 6.3 Pasni earthquake and its significance for future major earthquakes in the eastern Makran
<p>On 7th February 2017, a moment magnitude (M<sub>w</sub>) 6.3 earthquake rattled offshore Pasni in the eastern Makran and triggered a small tsunami. Using a combination of seismicity, multibeam bathymetry, seismic profile, InSAR measurements, and tide gauge observation, we conduct an in-depth investigation into the seismogenic structure, coseismic deformation, and tsunami characteristics of this event. Our results indicate that (1) the earthquake occurred on the shallow-dipping (3-4°) megathrust; (2) the megathrust co-seismically slipped 15 cm and caused ~2-4 cm ground subsidence and uplift at Pasni; (3) our tsunami modeling reproduces the observed 5-cm-high small tsunami waveforms. The Pasni earthquake rupture partially overlaps the 1851 and 1945 earthquake (M>8) slip patches, releasing estimated 3% and 7% of accumulative strain since then. With such stress perturbation, the Pasni earthquake could promote failure of megathrust in the future. This study calls for more preparedness in mitigating earthquake and associated hazards in the eastern Makran. </p>
Data from: 3D shear-wave velocity model of central Makran using ambient-noise adjoint tomography
<p>The Makran subduction zone is unique in its wide onshore thick accretionary prism, and a volcanic arc not parallel to the E-W trend of the Makran accretionary prism. To investigate the internal structure of the accretionary prism, the crustal nature of Jaz Murian Depression, and the trend of the buried trench we have calculated a 3D shear-wave velocity model for a region around the border between eastern and western Makran using ambient-noise adjoint tomography and data from IASBS/CAM Makran temporary seismic network. In close agreement with previous works, our velocity model shows that the onshore accretionary prism consists of a low-velocity zone in the south and a high-velocity zone in the north with an average thickness of accreted sediments of 22 and 30 km, respectively. The young age of the surface rocks of the high-velocity part of the prism suggests the presence of a significant volume of igneous rocks scraped from the subducting oceanic slab. The velocity model indicates a continental crust of ~40 km with a thick sedimentary cover of ~20 km for the eastern part of Jaz Murian Depression. The presence of a NE-SW trending low-velocity region at a depth interval of 40-60 km subparallel with the trend of the volcanic arc, intermediate-depth earthquakes, and geometry of the overriding plate might be related to the trend of the buried trench. This implies that the observed NE-SW trending volcanic arc might be related to the geometry of the buried trench and not the eastward reduction of the subduction angle.</p>
Data from: 3D shear-wave velocity model of central Makran using ambient-noise adjoint tomography
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FIGURE 5 in Cabdio occidentalis, a new species from Lake Mashkid basin and the Makran region (Teleostei: Danionidae)
FIGURE 5. Cabdio occidentalis, from top: BIAUBM 2-H, holotype, 77 mm SL; AJRPC 11, 71 mm SL; FSJF 4120, 65 mm SL, Iran: Sarbaz River.
FIGURE 1 in Cabdio occidentalis, a new species from Lake Mashkid basin and the Makran region (Teleostei: Danionidae)
FIGURE 1. Records of Cabdio occidentalis in Iran, red circle denotes type locality and black circles denotes additional occurrence points in Iran.
FIGURE 2 in Cabdio occidentalis, a new species from Lake Mashkid basin and the Makran region (Teleostei: Danionidae)
FIGURE 2. Phylogenetic reconstruction of the relationships of different Cabdio species based on the Maximum likelihood and Bayesian analysis of the mitochondrial DNA barcode region. Numbers near nodes are UFBoot/SH-aLRT/Posterior Probability values. The tree is drawn to scale with branch lengths depicting number of substitutions per site. The list of sequences is presented in Table 1.
Dataset for the "Widespread Aseismic Slip Along the Makran Megathrust Triggered by the 2013 Mw 7.7 Balochistan Earthquake" paper
<p>This dataset is used for the Widespread Aseismic Slip Along the Makran Megathrust Triggered by the 2013 Mw 7.7 Balochistan Earthquake paper. Containing the ascending and descending InSAR results processing by MintPy, and the processed observation and input files for BEAT.</p>
FIGURE 11 in Garra roseae, a new species from the Makran region in southern Iran (Teleostei: Cyprinidae)
FIGURE 11. Dorsal and ventral views; above: Garra rossica, VMFC GROS, 86 mm SL; Iran: spring Golbahar; below: Garra nudiventris, VMFC GND, 81 mm SL; Iran: qanat near Nehbandan.
FIGURE 10 in Garra roseae, a new species from the Makran region in southern Iran (Teleostei: Cyprinidae)
FIGURE 10. Above: Garra nudiventris, VMFC GND, 81 mm SL; Iran: Qanat near Nehbandan. Below: Garra rossica, VMFC GROS, 86 mm SL; Iran: spring Golbahar.
FIGURE 6 in Garra roseae, a new species from the Makran region in southern Iran (Teleostei: Cyprinidae)
FIGURE 6. Garra roseae, VMFC GR-P, paratypes; from above: 36 mm SL; 35 mm SL; 34 mm SL; 34 mm SL; Iran: stream Tang-e-Sarhe.
FIGURE 4 in Garra roseae, a new species from the Makran region in southern Iran (Teleostei: Cyprinidae)
FIGURE 4. Garra roseae, VMFC GR-P, paratypes; from above: 36 mm SL; 35 mm SL; 34 mm SL; 34 mm SL; Iran: stream Tang-e-Sarhe.
FIGURE 5 in Garra roseae, a new species from the Makran region in southern Iran (Teleostei: Cyprinidae)
FIGURE 5. Garra roseae, VMFC GR-P, paratypes; from above: 36 mm SL; 35 mm SL; 34 mm SL; 34 mm SL; Iran: stream Tang-e-Sarhe.
FIGURE 1 in Garra roseae, a new species from the Makran region in southern Iran (Teleostei: Cyprinidae)
FIGURE 1. Records of the Garra variabilis species group in Iran. See below for the sources of records the map is based on.
FIGURE 2 in Garra roseae, a new species from the Makran region in southern Iran (Teleostei: Cyprinidae)
FIGURE 2. Phylogenetic tree of mitochondrial COI barcode region rendered by Bayesian inference (BI). Numbers on branches indicate posterior probability values for BI and Maximum Likelihood (ML) bootstrap. Model of rate heterogeneity: Gamma with 4 categories Gamma shape alpha: 0.1905. Black solid bars right to the specimen labels indicate species delimitation results from mPTP followed by the results of the PTP approach as gray solid bars. The tree is drawn to scale with branch lengths depicting number of substitutions per site.
FIGURE 8. X in Morphological and molecular characterization of the Makran Glossogobius cf. giuris (Teleostei: Gobiidae) and the Glossogobius giuris species complex taxonomy
FIGURE 8. X-ray and caudal-fin skeleton (drawing) of Glossogobius cf. giuris from the Sarbaz River, Makran River System (ZM-CBSU N1064, 101.5 mm SL). Terminology is given in the text.
FIGURE 7 in Morphological and molecular characterization of the Makran Glossogobius cf. giuris (Teleostei: Gobiidae) and the Glossogobius giuris species complex taxonomy
FIGURE 7. Sensory papillae lines and head pores of Glossogobius cf. giuris based on ZM-CBSU G1-MK, 103 mm SL, from the Sarbaz River, Markarn River System (A, lateral view; B, ventral view). Terminology is given in the text.
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