Abstract
The hole reached 1350 m below the sea-floor. The various alteration minerals include chlorite, actinolite, pyrite, albite, sphene, quartz, epidote, sulphides, zeolites, anhydrite, clays and calcite. Alteration is controlled by permeability and primary mineralogy.-K.A.R.
Cite
CITATION STYLE
APA
Alt, J. C., Laverne, C., & Muehlenbachs, K. (1985). Alteration of the upper oceanic crust: mineralogy and processes in Deep Sea Drilling Project hole 504B, Leg 83. Initial Reports of the D.S.D.P., 83, 217–247. https://doi.org/10.2973/dsdp.proc.83.108.1985
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