Ore Deposits of the Guanajuato District, Mexico
The Guanajuato mining district is located in the central part of the state of Guanajuato, 475 kn1 northwest of Mexico City (Fig. 1). The district has an approximate length of 20 km and a width of 16 km, and includes the mining areas of La Luz to the west, Santa Rosa to the north, and Peregtina-El Cubo to the east (Fig. 2). The city of Guanajuato is located at the center of the district. Guanajuato can be reached by paved highways, railroad, or by commercial plane (by way of León airport, 62 km from Guanajuato city). The Torres-Cedros mine, which has the greatest production in the district, is located 3.2 km from the city and can be reached by a dirt road.
Figures & Tables
Mexican Silver Deposits
Much of the first day's route is spent in travelling in a southerly direction through desert basins to Chihuahua City (Fig. 1). Numerous ranges are visible from the roadside and some stops are scheduled for description of lithologies and structures, particularly where mapping has been accomplished. Of particular interest is the lower Cretaceous in Sierra del Presidio and Banco Lucero, Los Medanos (dune field), Sierra La Candelaria and Sierra El Kilo intrusions, and the Tertiary volcanic stratigraphy of Sierra Gallego (near El Sueco), Sierra El Nido, Sierra de La Campana, and Sierra Sacramento. The Sierra de Samalayuca, near the community of the same name, has been considered by some to be Early Jurassic or Paleozoic in age, and it consists of weakly-metamorphosed sediments in an anticlinal structure.
The underground visit to the manto and breccia-pipe deposits at the Potosí mine, West Camp, Santa Eulalia completes the day.
0.0 Buenos dias. Proceed north on Santa Fe Street.
0.1 Turn right on frontage road (Wyoming) and proceed eastward through 4 traffic lights.
0.9 Join I-10, travelJing east, passing Southern Pacific railroad yards.
2.2 Pass Southern Pacific railroad yards on right. Continue east on I-10; keep in right lane. At 9:00 is southern flank of Franklin Mountains, where Bliss Sandstone is overlain by Ordovician strata (Fig. 2), and the El Paso Group overlies a Precambrian (Red Bluff) crystalline complex. The tectonic style of the Franklin Mountains comprises a north-trending, west-dipping, tilted fault block typical of Basin and Range structure (see Lovejoy, 1980).
The Rio Grande Valley is aligned from northwest to southeast, but curves prominently between Cerro Cristo Rey and the Southern Franklin Mountains, forming El Paso del Norte. Between the Franklin Mountains and the Hueco Mountains (to the east) lies the Hueco Bolson; a relatively flat valley which is filled with sand and silts and is the major source of El Paso's water supply.
The Franklin Mountains range is linear, extending from its southern limit near central El Paso, north and slightly west for approximately 24 km, to a point about 6 km north of the Texas New Mexico boundary. The range is roughly 5 km wide. The highest point, North Franklin, or Cabeza de Vaca Peak, is approximlately 2,390 m above sea level. Precambrian igneous rocks comprise North Franklin Peak, making it the area of greatest structural relief in the state of Texas.
The oldest rocks exposed in