There are 14 spatial coverages corresponding to 12 records.
{
"404":{"id_local":"FR-18008901306731-2018-07-18","title_for_url":"Continental-weathering-as-a-driver-of-Late","title":"Continental weathering as a driver of Late Cretaceous cooling: new insights from clay mineralogy of Campanian sediments from the southern Tethyan margin to the Boreal realm"},
"405":{"id_local":"FR-18008901306731-2018-07-18-02","title_for_url":"Clay-mineralogical-and-geochemical-expressions-of","title":"Clay mineralogical and geochemical expressions of the \"Late Campanian Event\" in the Aquitaine and Paris basins (France): Palaeoenvironmental implications"},
"482":{"id_local":"FR-18008901306731-2019-08-08","title_for_url":"Mass-screening-for-Alveolar-echinococcosis-in","title":"Mass screening for Alveolar echinococcosis in south Gansu, China"},
"507":{"id_local":"FR-18008901306731-2020-08-21","title_for_url":"Quantitative-X-ray-mapping-of-brittle-shear-zones","title":"Quantitative X-ray mapping of brittle shear zones precursors"},
"509":{"id_local":"FR-18008901306731-2020-10-27","title_for_url":"Microprobe-analysis-on-a-brittle-shear-zone","title":"Microprobe analysis on a brittle shear zone precursor"},
"510":{"id_local":"FR-18008901306731-2020-10-27-02","title_for_url":"EBSD-mapping-of-shear-zones-strain-gradient","title":"EBSD mapping of shear zones strain gradient - seismic anisotropy"},
"511":{"id_local":"FR-18008901306731-2020-11-06","title_for_url":"EBSD-mapping-of-brittle-shear-zones-precursors","title":"EBSD mapping of brittle shear zones precursors"},
"512":{"id_local":"FR-18008901306731-2020-11-06-02","title_for_url":"EBSD-mapping-of-shear-zones-strain-gradient","title":"EBSD mapping of shear zones strain gradient - deformation mechanisms"},
"543":{"id_local":"FR-18008901306731-2021-06-09","title_for_url":"Suretta-nappe-shear-zones","title":"Suretta nappe shear zones"},
"589":{"id_local":"FR-18008901306731-2022-04-01-02","title_for_url":"Majors-traces-elements-and-strontium-isotopes","title":"Majors, traces elements and strontium isotopes (87Sr\/86Sr) of Cretaceous limestone and Quaternary marl - Jura Mountains"},
"590":{"id_local":"FR-18008901306731-2022-04-01-03","title_for_url":"Strontium-isotopic-ratio-87Sr-86Sr-of-waters","title":"Strontium isotopic ratio (87Sr\/86Sr) of waters from the Forbonnet peatland - Jura Mountains"},
"595":{"id_local":"FR-18008901306731-2022-04-11","title_for_url":"Pressure-Temperature-quantification-of","title":"Pressure-Temperature quantification of continental crustal hydration - Colorado Plateau"}
}
[
{"id":0,"name":"Europe","data":"404","proj":"WGS84","n":60,"e":30,"s":34,"w":-11,"fillColor":"rgba(255, 0, 0, 0.005)","strokeColor":"rgba(192, 0, 0, 0.8)"},
{"id":1,"name":"France","data":"405","proj":"WGS84","n":51.3334,"e":9.8334,"s":41.25,"w":-5.25,"fillColor":"rgba(255, 128, 0, 0.005)","strokeColor":"rgba(192, 96, 0, 0.8)"},
{"id":2,"name":"Sud de Gansu","data":"482","proj":"WGS84","n":34.6,"e":104.63,"s":34.48,"w":104.34,"fillColor":"rgba(255, 255, 0, 0.005)","strokeColor":"rgba(192, 192, 0, 0.8)"},
{"id":3,"name":"Zone de Neves - Fen\u00eatre des Tauern","data":"507","proj":"WGS84","n":46.9753449650407,"e":11.8223819704726,"s":46.9544923321588,"w":11.7794666262344,"fillColor":"rgba(128, 255, 0, 0.005)","strokeColor":"rgba(96, 192, 0, 0.8)"},
{"id":4,"name":"Zone de Neves - Fen\u00eatre des Tauern","data":"509","proj":"WGS84","n":46.9753449650407,"e":11.8223819704726,"s":46.9544923321588,"w":11.7794666262344,"fillColor":"rgba(0, 255, 0, 0.005)","strokeColor":"rgba(0, 192, 0, 0.8)"},
{"id":5,"name":"Zone de Neves - Fen\u00eatre des Tauern","data":"510","proj":"WGS84","n":46.9753449650407,"e":11.8223819704726,"s":46.9544923321588,"w":11.7794666262344,"fillColor":"rgba(0, 255, 128, 0.005)","strokeColor":"rgba(0, 192, 96, 0.8)"},
{"id":6,"name":"Massif de Monte Mucrone - Zone de Sesia","data":"510","proj":"WGS84","n":45.6384133642897,"e":7.95935153611936,"s":45.6222079276483,"w":7.93514728196897,"fillColor":"rgba(0, 255, 128, 0.005)","strokeColor":"rgba(0, 192, 96, 0.8)"},
{"id":7,"name":"Zone de Neves - Fen\u00eatre des Tauern","data":"511","proj":"WGS84","n":46.9753449650407,"e":11.8223819704726,"s":46.9544923321588,"w":11.7794666262344,"fillColor":"rgba(0, 255, 255, 0.005)","strokeColor":"rgba(0, 192, 192, 0.8)"},
{"id":8,"name":"Zone de Neves - Fen\u00eatre des Tauern","data":"512","proj":"WGS84","n":46.9753449650407,"e":11.8223819704726,"s":46.9544923321588,"w":11.7794666262344,"fillColor":"rgba(0, 128, 255, 0.005)","strokeColor":"rgba(0, 96, 192, 0.8)"},
{"id":9,"name":"Massif de Monte Mucrone - Zone de Sesia","data":"512","proj":"WGS84","n":45.6384133642897,"e":7.95935153611936,"s":45.6222079276483,"w":7.93514728196897,"fillColor":"rgba(0, 128, 255, 0.005)","strokeColor":"rgba(0, 96, 192, 0.8)"},
{"id":10,"name":"Spl\u00fcgen Pass","data":"543","proj":"WGS84","n":46.5082782774967,"e":9.337387919295,"s":46.5082782774967,"w":9.337387919295,"fillColor":"rgba(0, 0, 255, 0.005)","strokeColor":"rgba(0, 0, 192, 0.8)"},
{"id":11,"name":"Tourbi\u00e8re du Forbonnet (Frasne-Bouverans)","data":"589","proj":"WGS84","n":46.8274215834199,"e":6.17699432477821,"s":46.8227820925833,"w":6.17090034589637,"fillColor":"rgba(128, 0, 255, 0.005)","strokeColor":"rgba(96, 0, 192, 0.8)"},
{"id":12,"name":"Tourbi\u00e8re du Forbonnet (Frasne-Bouverans)","data":"590","proj":"WGS84","n":46.8274215834199,"e":6.17699432477821,"s":46.8227820925833,"w":6.17090034589637,"fillColor":"rgba(255, 0, 255, 0.005)","strokeColor":"rgba(192, 0, 192, 0.8)"},
{"id":13,"name":"Plateau du Colorado","data":"595","proj":"WGS84","n":39.0732225813367,"e":-106.334473192692,"s":34.0647954943912,"w":-110.904785692692,"fillColor":"rgba(255, 0, 128, 0.005)","strokeColor":"rgba(192, 0, 96, 0.8)"}
]
![[X]](img/btn/chk1.png)
chemistry, analytical
![[ ]](img/btn/chk0.png)
environmental sciences
