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91 results for “Pamir”

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zenodo44/100

Cosmogenic radionuclide and thermochronology data from the Tian Shan and northern Pamir

<p>The zip folder <em>Kudriavtseva_etal_TianShan_Repository</em> contains the following files and folders:</p> <p>The excel file <em>Kudriavtseva_SuppInfo-Tables_S1-S7&nbsp;</em>provides&nbsp;seven&nbsp;data tables with&nbsp;cosmogenic <sup>10</sup>Be, low-temperature thermochronology, and geospatial data from the&nbsp;Tian Shan and northern Pamir. These data tables form&nbsp;part of the Supporting Information for the study&nbsp;<em>&quot;Impact of Quaternary glaciations on denudation rates in north Pamir </em><strong>&ndash; </strong><em>T<em>ian Sh</em>an inferred from cosmogenic <sup>10</sup>Be and low-temperature thermochronology&quot; </em>by Kudriavtseva et al.</p> <p>The folders&nbsp;<em>Be10-glacial-correction </em>and <em>Be10-no_correction&nbsp;</em>include&nbsp;input files for calculating <sup>10</sup>Be-derived denudation rates using&nbsp;the open-source program CAIRN v.1 (Mudd et al., 2016) and shapefiles of drainage basins from the Tian Shan and northern Pamir. These data include original 10Be data from this study, as well as published 10Be data from Grin et&nbsp;al. (2018) and Charreau et al. (2023).</p> <p>The folder <em>Thermochronology_Data&nbsp;</em>includes two excel files summarizing published AFT and AHe data from the Tian Shan, input data for calculating exhumation&nbsp;rates using <em>age2exhume</em> MATLAB code (van der Beek &amp; Schildgen, 2023), and the resulting exhumation rates. Additionally, this folder contains two text files with the input AFT and AHe data; they&nbsp;can be directly imported into MATLAB.</p>

opencc-by-4.0Sep 2023View details →
zenodo40/100

Рис. 4. Раковины видов Melanoididae иЗ термальных источников: А – Melanoides pamiricus Lindholm иЗ теплого источника ДЖаушангоЗ (Памир), высота раковины 16 мм; В – M. shahdaraensis Starobogatov et Izzatullaev, иЗ теплого источника ДЖаушангоЗ, высота раковины 15 мм; С – M. kainarensis Starobogatov et Izzatullaev иЗ теплого источника ХадЖа-Кайнар (юго-восток Туркмении), высота раковины 23 мм. Фото З. ИЗЗатуллаева, 1976, 1980 гг. Fig. 4. Shells of the Melanoididae species from thermal springs: A – Melanoides pamiricus Lindholm, the hot spring Dzhaushangoz (Pamir), shell height 16 mm; B – M. shahdaraensis Starobogatov et Izzatullaev, the hot spring Dzhaushangoz, shell height 15 mm; C – M. kainarensis Starobogatov et Izzatullaev, the hot spring Khadzha-Kainar (south-eastern Turkmenistan). Photo by Z. Izzatullaev, 1976, 1980. in Patterns of ecology and life cycles of aquatic molluscs from Central Asia

Рис. 4. Раковины видов Melanoididae иЗ термальных источников: А – Melanoides pamiricus Lindholm иЗ теплого источника ДЖаушангоЗ (Памир), высота раковины 16 мм; В – M. shahdaraensis Starobogatov et Izzatullaev, иЗ теплого источника ДЖаушангоЗ, высота раковины 15 мм; С – M. kainarensis Starobogatov et Izzatullaev иЗ теплого источника ХадЖа-Кайнар (юго-восток Туркмении), высота раковины 23 мм. Фото З. ИЗЗатуллаева, 1976, 1980 гг. Fig. 4. Shells of the Melanoididae species from thermal springs: A – Melanoides pamiricus Lindholm, the hot spring Dzhaushangoz (Pamir), shell height 16 mm; B – M. shahdaraensis Starobogatov et Izzatullaev, the hot spring Dzhaushangoz, shell height 15 mm; C – M. kainarensis Starobogatov et Izzatullaev, the hot spring Khadzha-Kainar (south-eastern Turkmenistan). Photo by Z. Izzatullaev, 1976, 1980.

opencc-by-4.0Dec 2020View details →
zenodo40/100

Paleoseismology of the Northern Kongur Shan Extensional System, NE Pamir: Implications for Potential Irregular Earthquake Recurrence

<p>Data and code used in the manuscript submitted to JGR: Solid Earth, including:</p> <p>1. 0.1-m resolution DEM at the Alasai site</p> <p>2. Photomosaics of the lacustrine section and fault exposure</p> <p>3. Dataset on earthquake magnitude and liquefaction distance</p> <p>4. Matlab code for scarp degradation modeling</p> <p>5. Matlab code for Monte Carlo simulation of earthquake cycles</p>

opencc-by-4.0Jun 2024View details →
zenodo40/100

Fig. 13 in On The Study Of Fauna (Macroinvertebrates, Fish, Amphibians, Reptiles, Birds And Mammals) Of The Lower Course Of Shokhdara River Valley In Pamir, Mountain Bodakhshan, Tajikistan

Fig. 13. Total avifauna list versa the actually registered species; note: some species may be included in more than 1 type of occurrence.

opencc-by-4.0Jun 2024View details →
zenodo40/100

Fig. 10 in On The Study Of Fauna (Macroinvertebrates, Fish, Amphibians, Reptiles, Birds And Mammals) Of The Lower Course Of Shokhdara River Valley In Pamir, Mountain Bodakhshan, Tajikistan

Fig. 10. Himalayan agamas spotted along the rocks and mountain slopes along the course of Shokhdara River.

opencc-by-4.0Jun 2024View details →
zenodo40/100

Figures 2–5 in On the Chilopoda fauna of the Pamir Mts, Tajikistan, with notes on the highest records of chilopod species in Middle Asia

Figures 2–5. Habitats of Hessebius pervagatus Zalesskaja, 1978: 2, 3 – habitat at 3400 m (meadow along stream in mountain steppe, South Alichur Range), 4 – habitat at 4700–4900 (scree, surroundings of Koitezek Mountain Pass); 5 – female gonopod of H. pervagatus (ASU No. 588), laterally. Scale: 0.1 mm.

opencc-by-4.0Sep 2023View details →
zenodo40/100

Figure 5 in A new species and new subspecies of Eudiaphora Dubatolov, 1990 (Lepidoptera, Erebidae, Arctiinae) from Tien-Shan and Pamir ranges

Figure 5. Type locality of Eudiaphora tienshanensis sp. nov.: Sary-Chelek Region, 41.8200° N, 71.9722° E, Tien-Shan Range, Kyrgyzstan. (Photo: Vitaly M. Spitsyn).

opencc-by-4.0Aug 2019View details →
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Figure 4 in A new species and new subspecies of Eudiaphora Dubatolov, 1990 (Lepidoptera, Erebidae, Arctiinae) from Tien-Shan and Pamir ranges

Figure 4. Type locality of Eudiaphora turensis nozimdjoni ssp. nov.: ca. 8 km NW of Navobod village, 39.0739° N, 70.0983° E, Surkhob River valley, Pamir Range, Tajikistan. (Photo: Vitaly M. Spitsyn).

opencc-by-4.0Aug 2019View details →
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Figure 3 in A new species and new subspecies of Eudiaphora Dubatolov, 1990 (Lepidoptera, Erebidae, Arctiinae) from Tien-Shan and Pamir ranges

Figure 3. Maximum likelihood phylogeny of the genus Eudiaphora (violet filling) based on the COI dataset. Numbers near nodes are BS values. Tip labels: Species name | GenBank COI acc. number | Specimen locality. Blue labels indicate the new taxa under discussion. Our bPTP species delimitation model supported most of taxa as separate species-level units with exception of the branches colored red.

opencc-by-4.0Aug 2019View details →
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Figure 2 in A new species and new subspecies of Eudiaphora Dubatolov, 1990 (Lepidoptera, Erebidae, Arctiinae) from Tien-Shan and Pamir ranges

Figure 2. Male genitalia of Eudiaphora spp. A, B, C E. turensis turensis: general view of the male genitalia (A); juxta and saccus (B); aedeagus (C) D, E, F E. turensis nozimdjoni ssp. nov. (holotype): general view of the male genitalia (D); juxta and saccus (E); aedeagus (F) G, H, I E. tienshanensis sp. nov. (holotype): general view of the male genitalia (G); juxta and saccus (H); aedeagus (I). Scale bar = 1 mm. (Photos: Vitaly M. Spitsyn).

opencc-by-4.0Aug 2019View details →
zenodo40/100

Figure 1 in A new species and new subspecies of Eudiaphora Dubatolov, 1990 (Lepidoptera, Erebidae, Arctiinae) from Tien-Shan and Pamir ranges

Figure 1. Male specimens of Eudiaphora spp. A E. turensis turensis (Tajikistan, Khorog) B E. turensis nozimdjoni ssp. nov. (holotype) C E. tienshanensis sp. nov. (holotype). Scale bars = 10 mm. (Photos: Vitaly M. Spitsyn).

opencc-by-4.0Aug 2019View details →
zenodo40/100

Fig. 4 in The Middle Triassic scleractinia-like coral Furcophyllia from the Pamir Mountains

Fig. 4. Septal microarchitecture and traces of microstructure of Furcophyllia in transverse sections. A. Furcophyllia shaitanica sp. nov. Holotype, IGD 20556/23, upper Ladinian of the SE Pamirs, Republic of Tajikistan. Densely arranged septa with minute lateral granulations; centers of rapid accretion (CRA) are marked by dark dots. B. Furcophyllia septafindens (Volz, 1896), IPUM DOL/610, middle Carnian, St. Cassian Beds, Forcella di Sett Sass, Dolomites, Italy. Septa with relatively thick lateral granulations.

opencc-by-4.0Dec 2007View details →
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Fig. 3 in The Middle Triassic scleractinia-like coral Furcophyllia from the Pamir Mountains

Fig. 3. Septal apparatus of Furcophyllia in transverse sections. A–C, F. Furcophyllia shaitanica sp. nov. Holotype, GID 20556/23, upper Ladinian of the SE Pamirs, Republic of Tajikistan. A. Corallum with two calicular pits: this of the adult calice and a secondary one of newly forming calice (arrows); two parallel septa (s) pass from the area of the axial pit of the adult towards the area occupied by the new pit, limiting this area from two sides. B. The secondary axial pit. C. The section situated more proximally in comparison with the previous one, cutting the middle calicular part; only primary axial pit is to be observed with its radial arrangement of septa, any rudiments of the secondary pit are lacking. F. Peripheral region of the corallum with well developed septal brooms. D, E. Morphology of Furcophyllia septafindens (Volz, 1896); IPUM DOL/610, middle Carnian, St. Cassian Beds, Forcella di Sett Sass, Dolomites, Italy. D. The section cutting obliquely the corallum at the level near by the calicular floor showing elongated calicular fossa. Compare the subparallel arrangement of septa in the central part of the calice with radial one in F. shaitanica sp. nov. E. Endotheca in longitudinal section: note steeply sloping down, very low and extended dissepiments.

opencc-by-4.0Dec 2007View details →
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Fig. 2 in The Middle Triassic scleractinia-like coral Furcophyllia from the Pamir Mountains

Fig. 2. Peripheral facies zone in the Triassic of the South−Eastern Pamirs: succession of upper Ladinian–middle Carnian deposits in the Kattamardžanaj facies subzone (after Dronov 2001).

opencc-by-4.0Dec 2007View details →
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Fig. 1 in The Middle Triassic scleractinia-like coral Furcophyllia from the Pamir Mountains

Fig. 1. Facies zonation of the Triassic in the South−Eastern Pamirs (after Dronov and Melnikova 1985, modified).

opencc-by-4.0Dec 2007View details →
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GPS velocity field in the Pamir region in the Eurasian-fixed frame complied from our own results and previous studies

<p>The data file includes the GPS velocities with respect to the Eurasian frame in the Pamir, Tien Shan region.</p>

opencc-by-4.0Sep 2020View details →
zenodo36/100

Lithospheric deformation due to the 2015 M7.2 Sarez (Pamir) earthquake constrained by 5 years of space geodetic observations

<p>This zip file contains observations of postseismic surface deformation due to the 2015 Mw 7.2 Sarez earthquake derived from Sentinel-1 and ALOS-2 SAR data and GNSS positions over a time period of five years after the mainshock.</p>

opencc-by-4.0Apr 2022View details →
zenodo36/100

Figs 1–2 in A new species of the genus Epeolus Latreille, 1802 (Hymenoptera, Apoidea: Apidae) from the Pamirs, with a checklist of Central Asian species

Figs 1–2. Epeolus rasnitsyni sp. n., male, holotype. 1 – habitus, lateral view; 2 – original

opencc-by-4.0Sep 2021View details →
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Fig. 14 in On The Study Of Fauna (Macroinvertebrates, Fish, Amphibians, Reptiles, Birds And Mammals) Of The Lower Course Of Shokhdara River Valley In Pamir, Mountain Bodakhshan, Tajikistan

Fig. 14. Grey draft hamster.

opencc-by-4.0Jun 2024View details →
zenodo36/100

Fig. 9 in On The Study Of Fauna (Macroinvertebrates, Fish, Amphibians, Reptiles, Birds And Mammals) Of The Lower Course Of Shokhdara River Valley In Pamir, Mountain Bodakhshan, Tajikistan

Fig. 9. Young individual of spotted whip snake, road kill, Sebzor village.

opencc-by-4.0Jun 2024View details →

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