Subject area |
Earth Sciences |
More specific subject area |
Petrology, Geochemistry |
Type of data |
Microscopy images, tables, figures and graphs |
How data was acquired |
Major and trace element concentrations were determined on these sample tablets (Major elements as oxides in weight %, trace elements in ppm) using a sequentially operating, wavelength-dispersive X-ray fluorescence spectrometer (SIEMENS SRS 303 AS) on a volatile-free base. Rare Earth Elements was conducted by atomic emission spectroscopy, using inductively coupled plasma excitation at an ICP-AES (Jobin YVON Model 38 plus;Table 10, Table 11, Table 12, Table 13, Table 14, Table 15). 35 samples were analyzed and pulverized and by ICP-ES (oxides, Ba, Ni, Sc), and ICP-MS (trace and rare-earth elements) at ACME Laboratories, Vancouver, Canada.
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Data format |
Raw (photos), Analyzed, processed and filtered |
Experimental factors |
Thin sections were prepared, point-counted and photographed. 34 samples were crushed, pulverized, LOI (loss on ignition, the pre-annealed material was mixed with lithium tetraborate (Li2B4O7) in the ratio 2:1, melted at 1,400 ° C in a graphite crucible and poured into platinum pouring bowls. |
Experimental features |
Petrological and geochemical analysis of the rocks of The El Tranquilo Anticline |
Data source location |
El Tranquilo Anticline, Deseado Massif, Patagonia, Argentina |
Data accessibility |
Data available within this article |
Related research article |
Jenchen, U (2018).Petrography and geochemistry of the Triassic El Tranquilo Group, Deseado Massif, Patagonia, Argentina: Implications for provenance and tectonic setting. Journal of South American Earth Sciences, 88: 530-550. –https://doi.org/10.1016/j.jsames.2018.09.007[1]
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