ore_ctrl: | Cinnabar Occurs In Fractures And Breccia Along Fault Zones In Sandstone, Shale, And Siltstone Of The Puget Group. Mafic Rocks Intruded The Sediments, And All Were Subjected To Folding And Faulting Prior To Mineralization (Mackin, 1944, P. 8). The Shear Zone That Localizes Mineralization At The Barnum-Mcdonnell Deposit Has A Maximum Thickness Of 10 Ft. The Best Ore Is In Tuffaceous Sandstone (Huntting, 1956, P. 256). |
References: |
- Deposit:: GARD, L.M., JR., 1968, BEDROCK GEOLOGY OF THE LAKE TAPPS QUADRANGLE, PIERCE COUNTY, WASHINGTON: U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 388-B, 33 P., 2 PL.
- Deposit:: HUNTTING, M. T., 1956, INVENTORY OF WASHINGTON MINERALS-PART II, METALLIC MINERALS: WASHINGTON DIVISION OF MINES AND GEOLOGY BULLETIN 37, V. 1, 428 P.; V. 2, 67 P.
- Deposit:: MACKIN, J.H., 1944, RELATION OF GEOLOGY TO MINERALIZATION IN THE MORTON CINNABAR DISTRICT, LEWIS COUNTY, WASHINGTON: WASHINGTON DIVISION OF MINES AND MINING REPORT OF INVESTIGATIONS 6, 47 P., 2 PL.
- Deposit:: SCHASSE, H.W., COMPILER, 1987, GEOLOGIC MAP OF THE CENTRALIA QUADRANGLE, WASHINGTON: WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 87-11, 28 P., 1 PL.
- Deposit:: WDGER OF 90-18
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