cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.25582/data.2022-04.2473717/2131636
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473538/2131637
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473734/2131638
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474079/2131639
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474110/2131640
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474594/2131641
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474132/2131642
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474242/2131643
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474431/2131644
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474373/2131645
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474176/2131646
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473889/2131647
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473882/2131648
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474332/2131649
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474250/2131650
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473738/2131651
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474254/2131652
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474341/2131653
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473688/2131654
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474078/2131655
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474094/2131656
title: Data for EMSL Project 51287 from April 2022
DOI: 10.6084/m9.figshare.9746291
title: Subduction and collision processes between the North China and South China blocks constrained by the geochronology and geochemistry of the Wuguan Complex in the Qinling orogen, China

description: The Qinling orogen is a key area for understanding the processes of subduction and collision between the South China Block (SCB) and North China Block (NCB). The Wuguan Complex, distributed along the southern margin of the Shangdan suture zone, can provide important constraints on the age of collision between NCB and SCB and the tectonic evolution of the Qinling orogen in Late Paleozoic. Detrital zircons from meta-sedimentary rocks of the Wuguan Complex in the Danfeng-Shangnan area have an age spectrum with two main peaks at ~448 Ma and ~819 Ma, and two subordinate peaks at ~938 and ~1440 Ma, respectively, and are interpreted to have been derived from the North Qinling terrane (NQT). The petrographic and geochemical characteristics of the meta-sedimentary rocks indicate that they were deposited in a fore-arc basin along the southern margin of the NQT. The youngest detrital zircons yield a weighted mean age of 378 ± 3 Ma, indicating that the fore-arc deposition was continuing at least to this time, which implies that the Paleo-Qinling Ocean between the NCB and SCB was not finally closed until at least the late Devonian. In combination with regional data, we propose that sedimentary rocks of the Wuguan Complex might once have been a sequence of late Ordovician to late Devonian strata with intercalated mafic rocks, which has been dismembered by the later tectonic activity. It was metamorphosed during northward subduction of the Paleo-Qinling Ocean at ca. 320 Ma, and slowly cooled through ca. 350°C at ca. 247 Ma (muscovite <sup>40</sup>Ar/<sup>39</sup>Ar age). It has recorded the detailed processes of subduction and collision between the NCB and SCB.
DOI: 10.6084/m9.figshare.9746291.v1
title: Subduction and collision processes between the North China and South China blocks constrained by the geochronology and geochemistry of the Wuguan Complex in the Qinling orogen, China

description: The Qinling orogen is a key area for understanding the processes of subduction and collision between the South China Block (SCB) and North China Block (NCB). The Wuguan Complex, distributed along the southern margin of the Shangdan suture zone, can provide important constraints on the age of collision between NCB and SCB and the tectonic evolution of the Qinling orogen in Late Paleozoic. Detrital zircons from meta-sedimentary rocks of the Wuguan Complex in the Danfeng-Shangnan area have an age spectrum with two main peaks at ~448 Ma and ~819 Ma, and two subordinate peaks at ~938 and ~1440 Ma, respectively, and are interpreted to have been derived from the North Qinling terrane (NQT). The petrographic and geochemical characteristics of the meta-sedimentary rocks indicate that they were deposited in a fore-arc basin along the southern margin of the NQT. The youngest detrital zircons yield a weighted mean age of 378 ± 3 Ma, indicating that the fore-arc deposition was continuing at least to this time, which implies that the Paleo-Qinling Ocean between the NCB and SCB was not finally closed until at least the late Devonian. In combination with regional data, we propose that sedimentary rocks of the Wuguan Complex might once have been a sequence of late Ordovician to late Devonian strata with intercalated mafic rocks, which has been dismembered by the later tectonic activity. It was metamorphosed during northward subduction of the Paleo-Qinling Ocean at ca. 320 Ma, and slowly cooled through ca. 350°C at ca. 247 Ma (muscovite <sup>40</sup>Ar/<sup>39</sup>Ar age). It has recorded the detailed processes of subduction and collision between the NCB and SCB.
DOI: 10.25582/data.2022-04.2473651/2131657
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474515/2131658
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474578/2131659
title: Data for EMSL Project 51287 from April 2022
DOI: 10.6084/m9.figshare.9933269
title: Contrasting tectonic settings in Northern Chon Aike Igneous Province of Patagonia: subduction and mantle plume-related volcanism in the Marifil formation

description: The northern zone of the Chon Aike Igneous Province, located in the North Patagonian Massif, exhibits extensive outcrops of Jurassic volcanic rocks of the Marifil Formation. In the Arroyo Verde area, the initial volcanic stage of the Marifil Formation, that we denominate V0 (192.6 ± 2.5 Ma), includes coulées, megabreccias and lapilli tuffs assigned to plinian-type volcanism. This magmatism was generated by cold-wet-oxidized magmas that resemble those produced in active continental margins and volcanic arcs. The second stage, located unconformably over the first, includes welded lava-like ignimbrites, massive lapilli tuff and rhyolitic lava flow that resemble the Snake River-type volcanism. The magma that produces this volcanic stage exhibit the characteristics of hot-dry-reduced magmas emplaced in intraplate continental environments associated with continental rifting. This stage coincides with the V1 volcanic episode early recorded in the Marifil Formation.
DOI: 10.6084/m9.figshare.9981410.v1
title: Zircon U-Pb geochronology and geochemistry of Late Devonian–Carboniferous granitoids in NW Iran: implications for the opening of Paleo-Tethys

description: We present zircon U-Pb crystallization ages combined with bulk rock major and trace element geochemistry and Sr-Nd-Pb and zircon <i>in-situ</i> Hf isotopic compositions of the Amand and Moro granitoid intrusions in northwest Iran. The Amand and Moro plutons include granite and syeno-diorite with LA-ICP-MS U-Pb zircon ages of 367 ± 6.8 Ma and 351 ± 1.3 Ma, respectively, representative of Late Devonian-Early Carboniferous magmatic activity in NW Iran. Geochemical characteristics such as typical enrichments in alkalis, Nb, Zr, Ga and Y, depletion in P and Sr and fractionated REE patterns with high Ga/Al ratios and Eu negative anomalies are consistent with A-type magmatic signatures. The granitoids are classified as A<sub>2</sub>-type and within-plate granitoids. The bulk rock geochemistry (enrichments in Th, Nb and, high Th/Yb, Zr/Y ratios) along with low variation of <sup>143</sup>Nd/<sup>144</sup>Nd<sub>(i)</sub> and <sup>87</sup>Sr/<sup>86</sup>Sr<sub>(i)</sub> ratios and positive zircon εHf<sub>(t)</sub> support the role of a mantle plume component for the evolution of the Amand and Moro A-type granitoids in an extensional tectonic environment. In fitting with wider regional knowledge, this magmatism occurred during Paleo-Tethys opening in northern Gondwana.
DOI: 10.6084/m9.figshare.9896006
title: Early Paleozoic mantle evolution of East Kunlun Orogenic Belt in Qinghai, NW China: evidence from the geochemistry and geochronology of the Late Ordovician to Late Silurian mafic-ultramafic rocks in the Qimantag region

description: Subduction-related basaltic rocks in active continental margins should record information about the lithospheric mantle. Mafic rocks from the Qimantag region of the East Kunlun Orogenic Belt (EKOB), NW China, can be used to constrain the evolution of mantle sources. The Heishan basalts (445 Ma) and Xiarihamu gabbros (427 Ma) display distinct geochemical and isotopic features, with basalts yielding relatively lower Na<sub>2</sub>O+K<sub>2</sub>O (1.48–4.16 wt.%) and Mg<sup>#</sup> (0.50–0.57) than gabbros (Na<sub>2</sub>O+K<sub>2</sub>O = 2.96–4.07 wt.%, Mg<sup>#</sup> = 0.65–0.81). Although the basalts and gabbros show similar enrichment of LILE and depletion of HFSE, the gabbros have higher Th/Y and lower Sm/Th and Nb/U ratios than the basalts, indicative of derivation from a more enriched mantle source. The Heishan basalts have relatively positive εNd(t) values (+4.7 to +5.8) whereas the Xiarihamu gabbros have negative εNd(t) values ranging from −5.5 to −3.8. Crustal contamination played an insignificant role in the formation of the basalts and gabbros. Our data suggest that the basalts originated from a depleted mantle source, slightly enriched by subduction-related fluids, whereas the gabbros originated from an enriched mantle source. These findings support a subduction-related progressive lithospheric mantle enrichment model over ~20 Ma beneath the Qimantag region in the Early Palaeozoic.
DOI: 10.6084/m9.figshare.9896006.v1
title: Early Paleozoic mantle evolution of East Kunlun Orogenic Belt in Qinghai, NW China: evidence from the geochemistry and geochronology of the Late Ordovician to Late Silurian mafic-ultramafic rocks in the Qimantag region

description: Subduction-related basaltic rocks in active continental margins should record information about the lithospheric mantle. Mafic rocks from the Qimantag region of the East Kunlun Orogenic Belt (EKOB), NW China, can be used to constrain the evolution of mantle sources. The Heishan basalts (445 Ma) and Xiarihamu gabbros (427 Ma) display distinct geochemical and isotopic features, with basalts yielding relatively lower Na<sub>2</sub>O+K<sub>2</sub>O (1.48–4.16 wt.%) and Mg<sup>#</sup> (0.50–0.57) than gabbros (Na<sub>2</sub>O+K<sub>2</sub>O = 2.96–4.07 wt.%, Mg<sup>#</sup> = 0.65–0.81). Although the basalts and gabbros show similar enrichment of LILE and depletion of HFSE, the gabbros have higher Th/Y and lower Sm/Th and Nb/U ratios than the basalts, indicative of derivation from a more enriched mantle source. The Heishan basalts have relatively positive εNd(t) values (+4.7 to +5.8) whereas the Xiarihamu gabbros have negative εNd(t) values ranging from −5.5 to −3.8. Crustal contamination played an insignificant role in the formation of the basalts and gabbros. Our data suggest that the basalts originated from a depleted mantle source, slightly enriched by subduction-related fluids, whereas the gabbros originated from an enriched mantle source. These findings support a subduction-related progressive lithospheric mantle enrichment model over ~20 Ma beneath the Qimantag region in the Early Palaeozoic.
DOI: 10.6084/m9.figshare.9933269.v3
title: Contrasting tectonic settings in Northern Chon Aike Igneous Province of Patagonia: subduction and mantle plume-related volcanism in the Marifil formation

description: The northern zone of the Chon Aike Igneous Province, located in the North Patagonian Massif, exhibits extensive outcrops of Jurassic volcanic rocks of the Marifil Formation. In the Arroyo Verde area, the initial volcanic stage of the Marifil Formation, that we denominate V0 (192.6 ± 2.5 Ma), includes coulées, megabreccias and lapilli tuffs assigned to plinian-type volcanism. This magmatism was generated by cold-wet-oxidized magmas that resemble those produced in active continental margins and volcanic arcs. The second stage, located unconformably over the first, includes welded lava-like ignimbrites, massive lapilli tuff and rhyolitic lava flow that resemble the Snake River-type volcanism. The magma that produces this volcanic stage exhibit the characteristics of hot-dry-reduced magmas emplaced in intraplate continental environments associated with continental rifting. This stage coincides with the V1 volcanic episode early recorded in the Marifil Formation.
DOI: 10.6084/m9.figshare.9981410
title: Zircon U-Pb geochronology and geochemistry of Late Devonian–Carboniferous granitoids in NW Iran: implications for the opening of Paleo-Tethys

description: We present zircon U-Pb crystallization ages combined with bulk rock major and trace element geochemistry and Sr-Nd-Pb and zircon <i>in-situ</i> Hf isotopic compositions of the Amand and Moro granitoid intrusions in northwest Iran. The Amand and Moro plutons include granite and syeno-diorite with LA-ICP-MS U-Pb zircon ages of 367 ± 6.8 Ma and 351 ± 1.3 Ma, respectively, representative of Late Devonian-Early Carboniferous magmatic activity in NW Iran. Geochemical characteristics such as typical enrichments in alkalis, Nb, Zr, Ga and Y, depletion in P and Sr and fractionated REE patterns with high Ga/Al ratios and Eu negative anomalies are consistent with A-type magmatic signatures. The granitoids are classified as A<sub>2</sub>-type and within-plate granitoids. The bulk rock geochemistry (enrichments in Th, Nb and, high Th/Yb, Zr/Y ratios) along with low variation of <sup>143</sup>Nd/<sup>144</sup>Nd<sub>(i)</sub> and <sup>87</sup>Sr/<sup>86</sup>Sr<sub>(i)</sub> ratios and positive zircon εHf<sub>(t)</sub> support the role of a mantle plume component for the evolution of the Amand and Moro A-type granitoids in an extensional tectonic environment. In fitting with wider regional knowledge, this magmatism occurred during Paleo-Tethys opening in northern Gondwana.
DOI: 10.25582/data.2022-04.2474642/2131660
title: Data for EMSL Project 51287 from April 2022
DOI: 10.6084/m9.figshare.9933269.v2
title: Contrasting tectonic settings in Northern Chon Aike Igneous Province of Patagonia: subduction and mantle plume-related volcanism in the Marifil formation

description: The northern zone of the Chon Aike Igneous Province, located in the North Patagonian Massif, exhibits extensive outcrops of Jurassic volcanic rocks of the Marifil Formation. In the Arroyo Verde area, the initial volcanic stage of the Marifil Formation, that we denominate V0 (192.6 ± 2.5 Ma), includes coulées, megabreccias and lapilli tuffs assigned to plinian-type volcanism. This magmatism was generated by cold-wet-oxidized magmas that resemble those produced in active continental margins and volcanic arcs. The second stage, located unconformably over the first, includes welded lava-like ignimbrites, massive lapilli tuff and rhyolitic lava flow that resemble the Snake River-type volcanism. The magma that produces this volcanic stage exhibit the characteristics of hot-dry-reduced magmas emplaced in intraplate continental environments associated with continental rifting. This stage coincides with the V1 volcanic episode early recorded in the Marifil Formation.
DOI: 10.25582/data.2022-04.2474577/2131661
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474126/2131662
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473511/2131663
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474348/2131664
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473596/2131665
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474035/2131666
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474210/2131667
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474363/2131668
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474033/2131669
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473901/2131670
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473903/2131671
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474533/2131672
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473899/2131673
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473928/2131674
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474119/2131675
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474295/2131676
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473718/2131677
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474025/2131678
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473907/2131679
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474154/2131680
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474333/2131681
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474388/2131682
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474321/2131683
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474257/2131684
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474301/2131685
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473672/2131686
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474213/2131687
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473687/2131688
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473850/2131689
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474442/2131690
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473654/2131691
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474212/2131692
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473658/2131693
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473925/2131694
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473972/2131695
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474567/2131696
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474651/2131697
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473716/2131698
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473473/2131699
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474530/2131700
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473961/2131701
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474010/2131702
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473548/2131703
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474001/2131704
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473489/2131705
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474306/2131706
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473545/2131707
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474011/2131708
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473603/2131709
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473892/2131710
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473620/2131711
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474660/2131712
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473676/2131713
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474017/2131714
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473619/2131715
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474439/2131716
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474609/2131717
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474377/2131718
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474076/2131719
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473655/2131720
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473756/2131721
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474059/2131722
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473543/2131723
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474141/2131724
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473886/2131725
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474208/2131726
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473748/2131727
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474633/2131728
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473650/2131729
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474227/2131730
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473860/2131731
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474412/2131732
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474542/2131733
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473614/2131734
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473900/2131735
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474223/2131736
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473877/2131737
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474007/2131738
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474155/2131739
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473567/2131740
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474205/2131741
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474527/2131742
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474339/2131743
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474645/2131744
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474382/2131745
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474543/2131746
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2473945/2131747
title: Data for EMSL Project 51287 from April 2022
DOI: 10.25582/data.2022-04.2474107/2131748
title: Data for EMSL Project 51287 from April 2022