Magmatically folded and faulted schlieren zones formed by magma avalanching in the Sonora Pass Intrusive Suite, Sierra Nevada, California

Autor: Carmen Galindo, Scott R. Paterson, M. Leopold, Pablo H. Alasino, Jon F. Stanback, Katie E. Ardill

Publikováno v: E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET

The southwestern margin of the Late Cretaceous Sonora Pass Intrusive Suite, northern Sierra Nevada, California (USA), preserves a densely populated zone of magmatic structures that record dynamic magmatic layer formation and deformation (faulting and

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::52f1c521c05d3bce2593c1f4c2ffa7f2
https://doi.org/10.1130/ges02070.1