Petrography and mineral chemistry of Escalón meteorite, an H4 chondrite, México
PDF

Keywords

chondrite
H4 type
electron microprobe analyses
Chihuahua
Mexico

How to Cite

Reyes-Salas, A. M., Sánchez-Rubio, G., Altuzar-Coello, P., Ortega-Gutiérrez, F., Flores-Gutiérrez, D., Cervantes-de la Cruz, K., … Linares, C. (2018). Petrography and mineral chemistry of Escalón meteorite, an H4 chondrite, México. Revista Mexicana De Ciencias Geológicas, 27(1), 148–161. Retrieved from https://rmcg.unam.mx/index.php/rmcg/article/view/730

Citas en Dimensions Service

Share on

Abstract

The Escalón meteorite, a crusted mass weighing 54.3 g, was recovered near Zona del Silencio in Escalón, state of Chihuahua, México. The stone is an ordinary chondrite belonging to the high iron group H, type 4. Electron microprobe analyses of olivine (Fa18.1) and pyroxene (Fs16.5), phosphate, plagioclase, opaque phases, matrix and chondrule glasses are presented. The metal phases present are kamacite (6.08 % Ni), taenite (31.66 % Ni), high nickel taenite (50.01 % Ni) and traces of native Cu. The chondrules average apparent diameter measures 0.62 mm. X-ray diffraction pattern shows olivine, pyroxene and kamacite. Alkaline-type glass is found mainly in chondrules. This meteorite is a stage S3, shock-blackened chondrite with weathering grade W0.

PDF

Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 International License.

Downloads

Download data is not yet available.