| Fluid-inclusion evidence for the source of ore fluids for Mississippi Valley-type deposits in Missouri, Arkansas, Kansas, and Oklahoma, pp. 87-89, <In>, Martin, J.A., (ed.); Geology and mineral-resource assessment of the Springfield 1 [DEG] x 2 [DEG] quadrangle, Missouri, as appraised in September, 1985 |
Leach, D.L.; Rowan, E.L.; and Viets, J.G. |
U.S. Geological Survey, Bulletin no. 1942, 115 pages |
1991 |
N/A
|
| Genetic link between Ouachita foldbelt tectonism and the Mississippi Valley-type lead-zinc deposits of the Ozarks |
Leach, D.L.; and Rowan, E.L. |
Geology vol. 14, no. 11, pp. 931-935 |
1986 |
N/A
|
| Origin of late dolomite cement by CO2-saturated deep basin brines; evidence from the Ozark region, central United States; with suppl. data 91-10 |
Leach, D.L.; Plumlee, G.S.; Hofstra, A.H.; Landis, G.P.; Rowan, E.L.; and Viets, J.G. |
Geology vol. 19, no. 4, pp. 348-351 |
1991 |
N/A
|
| Precipitation of saddle dolomite cement by CO2; effervescence from upward-migrating basinal brines, (abstr.) |
Leach, D.L.; Plumlee, G.S.; Hofstra, A.H.; Landis, G.P.; Rowan, E.L.; and Viets, J.G. |
American Association of Petroleum Geologists, Bulletin vol. 74, no. 5, p. 701 |
1990 |
N/A
|