R Code Supporting the Manuscript: Using Stochastic Point Pattern Analysis to Track Regional Orientations of Magmatism During the Transition to Cenozoic Extension and Rio Grande Rifting, Southern Rocky Mountains
September 29, 2023
This repository contains code that supports ongoing research in the southern Rocky Mountains in Colorado and northern New Mexico. This region hosted intracontinental magmatism that developed during a tectonic transition from shortening (Laramide orogeny, ca. 75 to 40 Ma) through extension and rifting. The code in this repository presents a novel approach that uses stochastic weighted bootstrap simulations of a large set of geochronology data to better understand how the regional orientations of magmatism shifted during this time period.
Citation Information
Publication Year | 2023 |
---|---|
Title | R Code Supporting the Manuscript: Using Stochastic Point Pattern Analysis to Track Regional Orientations of Magmatism During the Transition to Cenozoic Extension and Rio Grande Rifting, Southern Rocky Mountains |
DOI | 10.5066/P9ONYGHN |
Authors | Joshua M Rosera |
Product Type | Software Release |
Record Source | USGS Digital Object Identifier Catalog |
USGS Organization | Geology, Energy & Minerals Science Center |
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Using stochastic point pattern analysis to track regional orientations of magmatism during the transition to cenozoic extension and Rio Grande rifting, Southern Rocky Mountains
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Assessing the mineral resources of the United States represents a core function of the Energy and Minerals Mission Area since the inception of the U.S. Geological Survey under the Organic Act of 1879. As reaffirmed by the Energy Policy Act of 2020, assessment of identified and undiscovered resources of critical mineral commodities continues to form a focal point of the Mineral Resources Program...
Using stochastic point pattern analysis to track regional orientations of magmatism during the transition to cenozoic extension and Rio Grande rifting, Southern Rocky Mountains
The southern Rocky Mountains in Colorado and northern New Mexico hosted intracontinental magmatism that developed during a tectonic transition from shortening (Laramide orogeny, ca. 75 to 40 Ma) through extension and rifting. We present a novel approach that uses stochastic weighted bootstrap simulations of a large set of new and historical geochronology data to better understand how regional anis
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Joshua Mark Rosera, Sean P. Gaynor, Alexey Ulianov, Urs Schaltegger