Abstract
A migratory magmatic arc developed in N Mexico between 140 and 18 m.y. ago. Calcic, calc-alkaline and alkaline rocks developed, accompanied by Cu, Mo, W, CaF2, Pb, Zn and Ag mineralization. -D.R.C.K. Dept. of Geological Sciences, Univ. of Texas at El Paso, El Paso, TX 79968, USA.
Cite
CITATION STYLE
APA
Clark, K. F., Foster, C. T., & Damon, P. E. (1982). Cenozoic mineral deposits and subduction-related magmatic arcs in Mexico. Geological Society of America Bulletin, 93(6), 533–544. https://doi.org/10.1130/0016-7606(1982)93<533:CMDASM>2.0.CO;2
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