Table T1. Summary of studies relating chert color to trace element composition.
Source article
Techniques
(elements analyzed)
Age of
chert
Location
Chert color range
Summary of results
Leudtke (1978)
INAA (Sm, Yb, Lu, La, Np/U, Sc, Na, Br, Ce, Th/P, Cr, Hf, Ba, Cs, Co, Rb, Eu, Sb, and Fe)
early Mississippian
Oceana County, Michigan
Gray to brown
1. Gray chalcedony had smaller proportions of all analyzed elements, except uranium and bromine.
2. Sandy brown chert had the greatest proportions of all elements, except uranium and bromine.
3. Gray chert is intermediate for all elements.
4. Chemical variations can exist within formations.

Frasier et al. (1972)
Flame AAS (Na2O and K2O)
late Cambrian to Mississippian
Illinois: Union County, Johnson County, Alexander County, Hardin County, McDonough County, Brown County, Kankakee County, Adams County
Black to gray to brown
1. Chemical composition varied mainly in the relative amounts of SiO2 and CaO.
XRF (TiO2, Al2O3, Fe2O3, MnO, MgO) Nevada: Hardin County
California: San Francisco (Twin Peaks)
Montana: Granite County, Near Old Mines
Ohio: Flint Ridge Park
Indiana: near Veedersburg

Hein et al. (1975)
X-ray mineralogy (quartz, calcite, smectite, hematite, illite, feldspar, barite, anhydrite, chlorite, apatite, gypsum) early Cretaceous to early Pliocene
Deep Sea Drilling Project Leg 62: Central North Pacific Ocean, Mid-Pacific Mountains, Hess Rise
Orange to brown to gray to black
1. The carbonate component of the chert is distinguished by high values of MgO, CaO, Mn, Ba, Sr, and Zr.
XRF (Mn, Ba, B, Zn, Ni, Y, Zn, Cu, Mo, Cr, Cu, SiO2, CaO, Al2O3, Fe2O3, CaO, Na2O, K2O, MgO)
2. Tuffaceous cherts have high values of K and Al, and commonly Zn, Mo, and Cr.
3. Pure cherts are characterized by high SiO2 and B.
4. High B percentages may be a good indication that the chert formed in an open-marine environment, isolated from terrigenous materials.

Notes: INAA = instrumental neutron activation analysis, AAS = atomic absorption spectroscopy, XRF = X-ray fluorescence.