File:BSE images of paralava with walstromite (B).png

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English: (A) aggregate of Ba-minerals between large rock-forming minerals of paralava, Zuk Tamrur. Frame shows a fragment magnified in Figure 3B; (B) walstromite intergrowing with zadovite and gurimite is partially replaced by pliniusite. Kalsilite, in enclaves containing walstromite, is intensively substituted by a mixture of hydrosilicates and zeolites; (C) one of the biggest poikilitic grain of walstromite with kalsilite inclusions and Ti- andradite-flamite (partly altered) eutectoid intergrowth, Zuk Tamrur; (D) Euhedral zadovite crystals in walstromite, zadovite partially substituted for fluorapatite, Gurim Anticline. Adr: andradite, Ap: fluorapatite, Brt: baryte, Cus: cuspidine, Ghl: gehlenite, Grm: gurimite, His: hydrosilicate, Pls: pliniusite, Rnk: rankinite, Tnr: tenorite, Wls: walstromite, Zdv: zadovite, Mgf: magnesioferrite, Kls: kalsilite. The image is published in an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
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Source https://www.mdpi.com/2075-163X/10/5/407/htm
Author Krzątała, Arkadiusz and Krüger, Biljana and Galuskina, Irina and Vapnik, Yevgeny and Galuskin, Evgeny
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current23:26, 7 March 2022Thumbnail for version as of 23:26, 7 March 20221,658 × 1,662 (761 KB)Yuanga (talk | contribs)File:BSE images of paralava with walstromite.png cropped 52 % horizontally, 52 % vertically using CropTool with precise mode.

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