Macusanite occurrence, age, and composition, Macusani, Peru

Bulletin of the Geological Society of America
By: , and 

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Abstract

Macusanite, originally believed to be a type of tektite because of its sculpture, is shown to be related to sillar of the Macusani region, Peru. K-Ar measurements establish identical Pliocene ages (4.2 m.y.) for macusanite and sillar and relate these deposits to the extensive ash flows of the southern Andes. These rocks are unique for glassy rocks in that lithium, boron, and arsenic contents are very high; cesium, rubidium, tellurium, fluorine, and tin are higher than normal; zinc, copper, chromium, and zirconium are lower than normal; and high-alumina minerals such as andalusite are present.

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Publication type Article
Publication Subtype Journal Article
Title Macusanite occurrence, age, and composition, Macusani, Peru
Series title Bulletin of the Geological Society of America
DOI 10.1130/0016-7606(1970)81[1539:MOAACM]2.0.CO;2
Volume 81
Issue 5
Year Published 1970
Language English
Publisher Geological Society of America
Description 8 p.
First page 1539
Last page 1546
Country Peru
City Macusani
Other Geospatial Andes Mountains
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