Mineral assessment tracts in Mohave county, Arizona

[Additional scientific data in this geographic area]

SB03: Skarn Cu (18b) (Mesozoic - Tertiary) , covers 4 % of this area
90%50%10%5%1%
330506060
SB06: Porphyry Cu (17) (Mesozoic - Tertiary) , covers < 0.1 % of this area
90%50%10%5%1%
00023
SB07: Porphyry Cu (17) (Mesozoic) , covers < 0.1 % of this area
90%50%10%5%1%
00112
SB08: Porphyry Cu (17) (Tertiary) , covers < 0.1 % of this area
90%50%10%5%1%
00012
SB09: Porphyry Cu (17) (Laramide) , covers 8 % of this area
90%50%10%5%1%
01223
SB10: Porphyry Cu (17) (Laramide) , covers 1.0 % of this area
90%50%10%5%1%
1251010
SB11: Porphyry Cu (17) (Laramide) , covers 2 % of this area
90%50%10%5%1%
00125
SB17: Porphyry Cu-Au (20c) (Laramide) , covers 35 % of this area
90%50%10%5%1%
01234
SB20: Polymetallic replacement + skarn Zn-Pb (19a + 18c) (Mesozoic - Tertiary) , covers 4 % of this area
90%50%10%5%1%
135710
SB24: Distal disseminated Ag-Au (19c) (Mesozoic - Tertiary) , covers 4 % of this area
90%50%10%5%1%
125710
SB25: Massive sulfide, kuroko (28a) (Proterozoic) , covers 1 % of this area
90%50%10%5%1%
01377
SB27: Epithermal vein, Comstock (25c) (Tertiary) , covers < 0.1 % of this area
90%50%10%5%1%
01222
SB28: Epithermal vein, Comstock (25c) (Tertiary) , covers < 0.1 % of this area
90%50%10%5%1%
01122
SB29: Epithermal vein, Comstock (25c) (Tertiary) , covers 15 % of this area
90%50%10%5%1%
1571015
SB32: Epithermal vein, quartz-alunite (25e) (Tertiary) , covers < 0.1 % of this area
90%50%10%5%1%
00234
SB33: Epithermal vein, quartz-alunite (25e) (Tertiary) , covers < 0.1 % of this area
90%50%10%5%1%
01245
SB34: Epithermal vein, quartz-alunite (25e) (Tertiary) , covers 15 % of this area
The number of undiscovered deposits in this tract was not estimated.
SB36: Hot-spring Au-Ag (25a) (Tertiary) , covers < 0.1 % of this area
90%50%10%5%1%
02468
SB38: Hot-spring Au-Ag (25a) (Tertiary) , covers < 0.1 % of this area
90%50%10%5%1%
01112
SB39: Hot-spring Au-Ag (25a) (Tertiary) , covers 15 % of this area
The number of undiscovered deposits in this tract was not estimated.