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Paleomagnetism of Sedimentary Rocks
Kenneth P. Kodama
€ 128.80
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Description for Paleomagnetism of Sedimentary Rocks
This book describes the paleomagnetism of sediments and sedimentary rocks, how sediments and sedimentary rocks become magnetized, and how the physical and chemical processes involved can affect the accuracy of paleomagnetism. Num Pages: 164 pages, Illustrations. BIC Classification: PHVG; RBG. Category: (P) Professional & Vocational. Dimension: 190 x 254 x 14. Weight in Grams: 592.
This book describes the paleomagnetism of sediments and sedimentary rocks, how sediments and sedimentary rocks become magnetized, and how the physical and chemical processes involved can affect the accuracy of paleomagnetism.
Read moreTopics covered include depositional and post-depositional remanence acquisition, the detection and correction of compaction-caused inclination shallowing, reduction diagenesis of magnetic minerals, chemical remagnetization, and rotation of remanence by...
Product Details
Publication date
2012
Publisher
John Wiley and Sons Ltd United Kingdom
Number of pages
164
Condition
New
Number of Pages
168
Format
Hardback
Place of Publication
Hoboken, United Kingdom
ISBN
9781444335026
SKU
V9781444335026
Shipping Time
Usually ships in 15 to 20 working days
Ref
99-15
About Kenneth P. Kodama
Ken Kodama is Professor of Earth and Environmental Sciences at Lehigh University. He has taught Earth sciences and conducted paleomagnetic and rock magnetic research with his students at Lehigh for the past 34 years. In his time away from paleomagnetism he enjoys playing music.
Reviews for Paleomagnetism of Sedimentary Rocks
“The book can be read easily and with great interest, particularly by readers being introduced to the subject. Kodama intelligently summarizes achievements in the field of sedimentary paleomagnetism, where he also plays an important role.” (Pure Appl. Geophys, 1 January 2015) “This easy-to-read volume is well illustrated, including 27 color plates, and it contains a useful glossary. Production quality is...
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