Structural evolution of the South American Andes

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ID: 299134
1947
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Abstract
A closer geological and tectonic study divides the Andean orogenic belt into two main geological provinces: a western province consisting of an extensive batholith of acid and semi-acid rocks, and an eastern province formed of sedimentary and metamorphic rocks of early Paleozoic to late Tertiary age.
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openalex_W2094407560 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Victor Oppenheim
Journal american journal of science
Year 1947
DOI
10.2475/ajs.245.3.158
URL
https://ajs.scholasticahq.com/article/61140.pdf
Keywords Keywords not found

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