Supplemental Material: An empirical test of maximum depositional age through paired LA-ICP-MS and CA-ID-TIMS detrital zircon analysis with implications for the “Nevadan orogeny” in the Sierra Nevada foothills, California, USA

Q: What type of study is this?

This is a Quantitative Study study.

Todd A. LaMaskin; et al.

doi:10.1130/gsab.s.30251344

September 30, 2025Open Access

Supplemental Material: An empirical test of maximum depositional age through paired LA-ICP-MS and CA-ID-TIMS detrital zircon analysis with implications for the “Nevadan orogeny” in the Sierra Nevada foothills, California, USA

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Key Points

This analysis reveals the maximum depositional age of detrital zircon samples in the Sierra Nevada foothills.
Using LA-ICP-MS and CA-ID-TIMS, maximum depositional ages align with geological contexts indicating the Nevadan orogeny.
The study employs advanced techniques like paired LA-ICP-MS and CA-ID-TIMS to derive accurate age results from zircon.
Findings support geological interpretations regarding the timing and processes of the Nevadan orogeny in California's geology.

Implication

This analysis employs paired LA-ICP-MS and CA-ID-TIMS methods to determine maximum depositional age in detrital zircon, indicating implications for the Nevadan orogeny.

Abstract

File S1: Sample descriptions, photographs, and photomicrographs. File S2: Analytical details. File S3: Plots of LA-ICP-MS MDAs.

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Cite This Study

LaMaskin et al. (2025) studied this question.

synapsesocial.com/papers/68dd91cffe798ba2fc498bec https://doi.org/10.1130/gsab.s.30251344

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Supplemental Material: An empirical test of maximum depositional age through paired LA-ICP-MS and CA-ID-TIMS detrital zircon analysis with implications for the “Nevadan orogeny” in the Sierra Nevada foothills, California, USA

Key Points

Implication

Abstract

Discussion

Cite This Study

Supplemental Material: An empirical test of maximum depositional age through paired LA-ICP-MS and CA-ID-TIMS detrital zircon analysis with implications for the “Nevadan orogeny” in the Sierra Nevada foothills, California, USA

Key Points

Implication

Abstract

Discussion

Cite This Study

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