Zonal Weathering of a Hornblende Gabbro

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Hornblende Gabbro Sill Complex at Onion Valley, California, and a Mixing Origin for the Sierra Nevada Batholith

The steep crest of the Sierra Nevada, Califor-nia, near Onion Valley, exposes natural cross sections through a mafic intrusive complex that formed as part of the Mesozoic Sierra Nevada batholith. Sheeted sills of hornblende gabbro to hornblende diorite, individually as thick as 1.5 m, form the upper 200 to 300 m of the complex. Thicker, multiply-injected sills, as well as mafic stocks, lie unde...

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ژورنال

عنوان ژورنال: The Journal of Geology

سال: 1916

ISSN: 0022-1376,1537-5269

DOI: 10.1086/622318