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.v1

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

The analysis reveals significant insights into the maximum depositional age using detrital zircon.
Key evidence includes paired LA-ICP-MS and CA-ID-TIMS measurements contributing to the understanding of geological history.
Methodology incorporates paired LA-ICP-MS and CA-ID-TIMS approaches for accurate sedimentary age assessment.
Implications suggest enhanced understanding of the Nevadan orogeny and its geological effects in California's Sierra Nevada foothills.

Implication

This analysis demonstrates maximum depositional age using LA-ICP-MS and CA-ID-TIMS in detrital zircon samples, highlighting the significance for understanding 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/68dd91cffe798ba2fc498ba6 https://doi.org/10.1130/gsab.s.30251344.v1

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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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