About This Item
- Full TextFull Text(subscription required)
- Pay-Per-View PurchasePay-Per-View
Purchase Options Explain
Share This Item
The validity of boron as a salinity index has been established by numerous studies over the past 2 decades. It is known that all the major clay minerals may contain boron which can be correlated with paleosalinity. However, under given conditions, illites will contain the most boron and kaolinites the least. Montmorillonites and probably chlorites are intermediate.
Published data indicate that a detrital clay will adsorb boron from solution, fix it at the surface, and later incorporate it within the structure. For seawater systems, this boron uptake can be expressed as a Freundlich adsorption isotherm, as log B = C1 log S + C2, where B = boron uptake (ppm), S = salinity of the water (^pmil), and C1, C2 = constants, dependent on the particular clay.
Factors other than salinity that affect boron content are inherited boron, clay mineralogy, grain size, and crystallinity of the clay minerals.
Sufficient independent data were available to use an adsorption isotherm to calculate paleosalinities for a kaolinitic Tertiary shale in Nigeria. The constants necessary for calibration of the isotherm were evaluated as:
Inherited "kaolinite boron," O; "Kaolinite boron" uptake at 1 ^pmil salinity 1.3 ppm (C2 = 0.11); and "Kaolinite boron" uptake at 35 ^pmil salinity 65 ppm (C1 = 1.28).
Boron concentrations, related to kaolinite, were converted graphically to paleosalinities from a log-log calibration curve with the use of these values. Paleosalinities determined in this manner are in good agreement with independent faunal interpretations.
Pay-Per-View Purchase Options
The article is available through a document delivery service. Explain these Purchase Options.
|Protected Document: $10|
|Internal PDF Document: $14|
|Open PDF Document: $24|
Members of AAPG receive access to the full AAPG Bulletin Archives as part of their membership. For more information, contact the AAPG Membership Department at [email protected].