Magnetic and mineralogical properties of salt rocks from the Zechstein of the Northern German Basin. Issue 3 (11th January 2017)

• Record Type: Journal Article
• Authors: Heinrich, Frances C.; Schmidt, Volkmar; Schramm, Michael; Mertineit, Michael
• Is Part Of: Geophysical journal international. Volume 208:Issue 3(2017:Mar.)
• Page Start: 1811
• Page End: 1831
• Publication Date: 2017-01-11
• Subjects: Magnetic mineralogy and petrology -- Rock and mineral magnetism; Geophysics -- Periodicals; 550
• DOI: 10.1093/gji/ggw488
• Languages: English
• ISSNs: 0956-540X

Abstract

Abstract: Magnetic properties of rocks are often studied to characterize composition and fabric of rocks. For salt rocks, the basic relationships between their magnetic properties and composition, which are necessary to interpret rock magnetic data, are not yet established. Therefore, we studied different types of natural salt rock and pure salt minerals. We measured their magnetic properties (magnetic susceptibility, isothermal remanent magnetization acquisition curves, first-order reversal curve diagrams and temperature-dependent magnetic susceptibility) and used analytical methods such as microscopy, X-ray diffraction and inductively coupled plasma atomic emission spectroscopy to understand the relationship between magnetic properties and mineralogy. Salt rocks mainly consist of the diamagnetic minerals halite, carnallite, sylvine and anhydrite with negative magnetic susceptibilities. The magnetic susceptibilities of pure synthetic NaCl and KCl single crystals, show values of −14.5 × 10 −6 and −13.5 × 10 −6 SI, respectively. In contrast, in natural salt rocks higher magnetic susceptibility values were measured. The magnetic susceptibility of the samples investigated in this study shows a general increase from light rock salt (maximum −10 × 10 −6 SI) over carnallitite (maximum 134 × 10 −6 SI) to red sylvinite (maximum 270 × 10 −6 SI). Whole rock analyses suggest that increased magnetic susceptibility can be attributed to paramagnetic and ferromagnetic minerals that are contained within the insoluble residue. The magnetic susceptibility is mainly controlled by magnetite and phyllosilicates. Its measurement can therefore be used to detect subtle changes in the content of these minerals.