Dataset for: Observations on feldspathic glass in the shergottites Northwest Africa (NWA) 12241, NWA 15628, and Dhofar 019: Implications for the origin of “maskelynite”

Document Type

Dataset

Publication Date

2026

Abstract

Maskelynite, here referred to as feldspathic glass, is the most abundant high-pressure phase produced by shock in extraterrestrial rocks, but controversies over its formation have limited its utility. It shows features that are in line with both melt and solid-state transformation models, thereby leading to major uncertainties about its significance. Here, we propose a new model (the “hybrid model”) for the formation of maskelynite  that explains its behavior based on new findings. Furthermore, we explore the utility of using maskelynite to infer shock-durations with this proposed model. Using best estimates of applicable shock temperatures, inferred shock durations are 0.23 ± 0.17 ms, 0.81 ± 0.11 ms, and 26.9 ± 2.2 ms for Northwest Africa (NWA) 12241, Dho 019, and NWA 15628, respectively. These values are comparable to literature estimates of ~1-100 ms for shergottites.

Description

This data supports an article being published in Meteoritics and Planetary Science.

Data include information about the samples that were studied, the chemical compositions of phases, linescan profile widths, averaged EBSD data, and a summary table detailing feldspathic glass and the models they satisfy.

Rights

This work is marked with CC0 1.0 Universal

DOI

10.15760/geology-data.10

Persistent Identifier

https://archives.pdx.edu/ds/psu/44656

Anim and Ruzicka Data Tables.csv (19 kB)
csv. file_7 tables _Observations on feldspathic glass

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