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Dataset for "Adjoint Waveform Tomography for Crustal and Upper Mantle Structure the Middle East and Southwest Asia for Improved Waveform Simulations Using Openly Available Broadband Data"
<p>This dataset contains the MESWA (Middle East and Southwest Asia) seismic model and auxiliary data used in the creation of the model (Rodgers, 2023). MESWA is a three-dimensional model of the seismic properties of crust and upper mantle of the Middle East and Southwest Asia. The MESWA model is provided in NetCDF format (readable by for example, <em>xarray</em>, Hoyer & Hamman, <a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2021JB022930#jgrb55516-bib-0057">2017</a>) and HDF5 format for viewing with <em>ParaView</em> (Ahrens et al., <a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2021JB022930#jgrb55516-bib-0002">2005</a>) and interaction with <em>Salvus</em> (Afanasiev et al., <a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2021JB022930#jgrb55516-bib-0001">2019</a>). </p> <p> </p> <p>Also included are the earthquake source parameters for all 327 Global Centroid Moment Tensor events considered in this study in ASCII text format. Also included are lists of the selected 192 inversion events and 66 validation events in ASCII text format. Lastly, we include a list of all receivers used in the creation and validation of MESWA. This is a simple ASCII file with the event name and receiver name (composed of the network_code and station_code).</p> <p> </p> <p>The following table provides a listing of the files in the dataset:</p> <table> <tbody> <tr> <td> <p><strong>File</strong></p> </td> <td> <p><strong>Description</strong></p> </td> </tr> <tr> <td> <p>MESWA.nc</p> </td> <td> <p>MESWA model in NetCDF format</p> </td> </tr> <tr> <td> <p>MESWA.h5</p> </td> <td> <p>MESWA model in HDF5 format, used by Salvus</p> </td> </tr> <tr> <td> <p>MESWA.xmdf</p> </td> <td> <p>Auxiliary file for MESWA.h5, used to import model into Paraview</p> </td> </tr> <tr> <td> <p>events_project.csv</p> </td> <td> <p>Table of event source parameters for all 327 events considered in the project</p> </td> </tr> <tr> <td> <p>inversion_events_192.csv</p> </td> <td> <p>Table of 192 inversion events </p> <p>(ASCII comma separated value)</p> </td> </tr> <tr> <td> <p>validation_events_66.csv</p> </td> <td> <p>Table of 66 validation events </p> <p>(ASCII comma separated value)</p> </td> </tr> <tr> <td> <p>events_receivers_inversion.csv</p> </td> <td> <p>Table of waveform (event-receiver-channel) data used in the inversion (ASCII comma separated value)</p> </td> </tr> <tr> <td> <p>events_receivers_validation.csv</p> </td> <td> <p>Table of waveform (event-receiver-channel) data used in the validation (ASCII comma separated value)</p> </td> </tr> </tbody> </table> <p> </p> <p> </p> <p><strong>References</strong></p> <p>Afanasiev, M, C Boehm, M van Driel, L Krischer, M Rietmann, DA May, MG Knepley, and A Fichtner (2019). Modular and flexible spectral-element waveform modelling in two and three dimensions, <em>Geophys. J. Int.</em>, 216(3), 1675–1692, doi: 10.1093/gji/ggy469</p> <p> </p> <p>Ahrens, J., Geveci, B., & Law, C. (2005). Paraview: An end-user tool for large data visualization. <em>The Visualization Handbook</em>, 717(8). <a href="https://doi.org/10.1016/b978-012387582-2/50038-1">https://doi.org/10.1016/b978-012387582-2/50038-1</a></p> <p> </p> <p>Hoyer, S., & Hamman, J. (2017). Xarray: N-D labeled arrays and datasets in Python. <em>Journal of Open Research Software</em>, 5(1). <a href="https://doi.org/10.5334/jors.148">https://doi.org/10.5334/jors.148</a></p> <p> </p> <p>Rodgers, A. (2023). Adjoint Waveform Tomography for Crustal and Upper Mantle Structure the Middle East and Southwest Asia for Improved Waveform Simulations Using Openly Available Broadband Data, technical report, LLNL-TR- 851939.</p> <p> </p> <p><strong>Acknowledgements</strong></p> <p>This project was support by Lawrence Livermore National Laboratory’s Laboratory Directed Research and Development project 20-ERD-008 and the National Nuclear Security Administration. This work was performed under the auspices of the U.S. Department of Energy by Lawrence Livermore National Laboratory under Contract DE-AC52-07NA27344. LLNL-MI-852402</p> <p> </p>
FIG. 7 in A new species of Tungurictis Colbert, 1939 (Carnivora, Hyaenidae) from the middle Miocene of Junggar Basin, northwestern China and the early divergence of basal hyaenids in East Asia
FIG. 7. — Tungurictis small sp., IVPP V 11497, left dentary fragment with m1 and m2 alveolus. A, stereo photos of occlusal view; B, lingual view; C, buccal view. Scale bars: 10 mm.
FIG. 5 in A new species of Tungurictis Colbert, 1939 (Carnivora, Hyaenidae) from the middle Miocene of Junggar Basin, northwestern China and the early divergence of basal hyaenids in East Asia
FIG. 5. — Tungurictis peignei, n. sp., IVPP V 25222, holotype, right dentary with p2-m2 (A, stereo photos, occlusal view, C, lingual, and D, buccal views) and IVPP V 11493, left dentary with p2-m1 (B, stereo photos, occlusal view; E, lingual view; F, buccal views). Scale bars: 10 mm.
FIG. 4 in A new species of Tungurictis Colbert, 1939 (Carnivora, Hyaenidae) from the middle Miocene of Junggar Basin, northwestern China and the early divergence of basal hyaenids in East Asia
FIG. 4. — Tungurictis peignei, n. sp., IVPP V 25222, holotype, isolated right I3, mesial view (A), right upper canine, buccal view (B), left P1, and left maxilla with P3-4 (C, stereo photos of occlusal view; D, buccal view). Scale bar: 10 mm.
Fig. 1 in A new Allium L. species from middle Asia
Fig. 1: Distribution of A. filidens alliance in Middle Asia. Black circle – A. rinae sp. nov. Black square – A. fritschii F. O. KHASS. & IENGAL. Black line – A. filidens REGEL
Fig. 4 in Middle Miocene bovids from Mae Moh Basin, Northern Thailand: The first record of the genus Eotragus from Southeast Asia
Fig. 4. Right astragalus of the bovid mammals, Eotragus lampangensis sp. nov., UPP MM-75 (A) and Eotragus clavatus (Gervais, 1850), MNHN Sa 2662 (B) middle Miocene of Sansan (France), in dorsal (A1, B1), lateral (A2, B2), medial (A3, B3), and plantar (A4, B4) views.
Fig. 3 in Middle Miocene bovids from Mae Moh Basin, Northern Thailand: The first record of the genus Eotragus from Southeast Asia
Fig. 3. Dental remains of the bovid mammals, Eotragus lampangensis sp. nov. (A–F, H, I) and Bovidae gen. et sp. indet. (G) from the the middle Miocene of Mae Moh Basin, Thailand. A. UPP MM-57, left DP3 in occlusal view. B. UPP MM-71, left M3 in occlusal (B 1) and labial (B 2) views. C. UPP MM-72, right p2 in occlusal (C 1) and lingual (C 2) views. D. UPP MM-66, right m1 in occlusal (D 1) and labial (D 2) views. E. UPP MM-62, fragmentary left mandible with p4 and m1 in occlusal (E 1) and lingual (E 2) views. F. UPP MM-73, left m2 in lingual (F 1), occlusal (F 2), and labial (F 3) views. G. UPP MM-76, left m3 in occlusal view. H. UPP MM-67, right m3 in occlusal view. I. UPP MM-74, right m3 in occlusal view.
Fig. 2 in Middle Miocene bovids from Mae Moh Basin, Northern Thailand: The first record of the genus Eotragus from Southeast Asia
Fig. 2. Cranial appendage remains of the bovid mammal Eotragus from the middle Miocene of Mae Moh Basin, Thailand, in anterior (A1–D1), medial (A2–D2), lateral (A3–D3), and posterior (A4–D4) views, and basal cross sections (A5–D5, dashed lines indicate broken areas). A. Eotragus lampangensis sp. nov., holotype, UPP MM-68, left horn core. B–D. Eotragus cf. lampangensis. B. UPP MM-29, right horn core. C. UPP MM-55, partial fragment of right horn core with pedicle. D. UPP MM-56, fragmentary right horn core. The basal cross sections (B5, C5, and D5) are oriented in the same direction.
Fig. 1 in Middle Miocene bovids from Mae Moh Basin, Northern Thailand: The first record of the genus Eotragus from Southeast Asia
Fig. 1. Map of Thailand showing the location of the Mae Moh Basin (A). Map of intermontane basins showing the location of mammal-bearing fossil localities (B).
Fig. 3 in New species and records of Quedius rove beetles (Coleoptera, Staphylinidae, Staphylininae) from Middle Asia
Fig. 3. Quedius viator sp. nov., holotype (ZIN). A. Habitus. B–D. Aedeagus. B. From parameral side. C. Apical portion of paramere (underside). D. Lateral view. E. Sternite VIII. F. Tegite X. G. Sternite IX. Scale bars: A = 1 mm; B–G = 0.5 mm..
Fig. 2 in New species and records of Quedius rove beetles (Coleoptera, Staphylinidae, Staphylininae) from Middle Asia
Fig. 2. Distribution map showing the type localities of Quedius gissaricus sp. nov. (red circle) and Q. viator sp. nov. (violet circle).
Fig. 1 in New species and records of Quedius rove beetles (Coleoptera, Staphylinidae, Staphylininae) from Middle Asia
Fig. 1. Quedius gissaricus sp. nov., holotype (ZIN). A. Habitus (interocular punctures indicated by red arrows). B–D. Aedeagus. B. From parameral side. C. Apical portion of paramere (underside). D. Median lobe (laterally). E. Sternite VIII. Scale bars: A =1 mm; B–E = 0.5 mm.
Figure 1. Pomerantzia benhami Price, 1974 in First record of the family Pomerantziidae (Acari: Trombidiformes) from Middle East, with recording of two species for the first time from Asia
Figure 1. Pomerantzia benhami Price, 1974 – Dorsal (left) and ventral (right) view of body and dorsolateral view of the chelicerae (center).
Figure 4 in First record of the family Pomerantziidae (Acari: Trombidiformes) from Middle East, with recording of two species for the first time from Asia
Figure 4. Apomerantzia kethleyi (Price, 1975) – A. Palp; B. Leg I (including ventral aspect of tarsal terminus in right); C. Leg II; D. Leg III; E. Leg IV.
Рис. 1. А – р. Зарафшан в среднем течении (предгорнаЯ река); В – р. Зарафшан в ниЖнем течении (равниннаЯ река). Фото Н. РуЗикуловой, 2019 г. Fig. 1. А – the Middle Zarafshan River (submountain river); B – the Lower Zarafshan River (lowland river). Photo by N. Ruzikulova, 2019. in Patterns of ecology and life cycles of aquatic molluscs from Central Asia
Рис. 1. А – р. Зарафшан в среднем течении (предгорнаЯ река); В – р. Зарафшан в ниЖнем течении (равниннаЯ река). Фото Н. РуЗикуловой, 2019 г. Fig. 1. А – the Middle Zarafshan River (submountain river); B – the Lower Zarafshan River (lowland river). Photo by N. Ruzikulova, 2019.
Figs 203-206 in A revision of the Sunius species of the Western Palaearctic region and Middle Asia (Coleoptera: Staphylinidae: Paederinae)
Figs 203-206: Sunius pennatus nov.sp. (203-205) and S. basalis (REITTER), syntype (206): (203, 206) forebody; (204) aedeagus in lateral view; (205) internal structures of aedeagus in lateral view. Scale bars: 206: 0.5 mm; 203: 0.2 mm; 204-205: 0.1 mm.
Figs 198-202 in A revision of the Sunius species of the Western Palaearctic region and Middle Asia (Coleoptera: Staphylinidae: Paederinae)
Figs 198-202: Sunius inflexus nov.sp.: (198) forebody; (199) aedeagus in lateral view; (200) internal structures of aedeagus in lateral view; (201) male sternite VII; (202) male sternite VIII. Scale bars: 198, 201-202: 0.2 mm; 199-200: 0.1 mm.
Map 23 in A revision of the Sunius species of the Western Palaearctic region and Middle Asia (Coleoptera: Staphylinidae: Paederinae)
Map 23: Distributions of species of the S. viator group in Tajikistan, based on examined records: Sunius wrasei (SCHÜLKE) (filled square), S. inflexus nov.sp. (open circle), S. bohaci nov.sp. (filled circle), and S. pennatus nov.sp. (open square). The territory of Tajikistan is highlighted to facilitate geographic recognition.
Figs 193-197 in A revision of the Sunius species of the Western Palaearctic region and Middle Asia (Coleoptera: Staphylinidae: Paederinae)
Figs 193-197: Sunius bohaci nov.sp.: (193) forebody; (194) aedeagus in lateral view; (195) internal structures of aedeagus in lateral view; (196) male sternite VII; (197) male sternite VIII. Scale bars: 193, 196-197: 0.2 mm; 194-195: 0.1 mm.
Figs 173-176 in A revision of the Sunius species of the Western Palaearctic region and Middle Asia (Coleoptera: Staphylinidae: Paederinae)
Figs 173-176: Sunius wrasei (SCHÜLKE), holotype: (173) habitus; (174) forebody; (175-176) aedeagus in lateral and in ventral view. Scale bars: 173-174: 1.0 mm; 175-176: 0.2 mm.
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