An introduction to the use of thin sections in the study of petrography—the scientific description of rocks. It covers all rock types—igneous, sedimentary and metamorphic—and provides readers with an excellent overview of the subject.
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Most Helpful Customer Reviews
9 of 10 people found the following review helpful:
1.0 out of 5 stars
MacKenzie produced a better text with C. Guilford,
By A Customer
This review is from: A Color Atlas of Rocks and Minerals in Thin Section (Paperback)
This book is overpriced and almost useless. It only serves as eye candy for someone with exposure to the petrographic microscope. Outside of pictures it contains terse explanations and alot of blank wasted space.
5 of 5 people found the following review helpful:
1.0 out of 5 stars
Avoid confusion!,
By Peter A Selkin (San Diego, CA United States) - See all my reviews
This review is from: A Color Atlas of Rocks and Minerals in Thin Section (Paperback)
I agree with the reviewer from Fairbanks: this book should not be confused with the Mackenzie and Guilford atlas. The Atlas of *Rocks* and Minerals tries to be too comprehensive (by including both rocks and minerals) and in doing so has lost all of the information about less common and accessory minerals that was in the Mackenzie and Guilford text. Of course, much of what's in both books is now available on the Web, but it's still hard to find large format color photos like the ones in Mackenzie and Guilford. Another (less expensive) alternative is A.R. Philpotts' "Petrography of Igneous and Metamorphic Rocks." In my experience as a student and then a TA in a mineralogy course, Philpotts' book does a better job of pointing out the distinctive characteristics of minerals than do the photographic atlases.
2 of 2 people found the following review helpful:
5.0 out of 5 stars
An Excellent book,
By
This review is from: A Color Atlas of Rocks and Minerals in Thin Section (Paperback)
The book is written in a consise and well laid out manner. As the previous writer stated, the colour photos are priceless and are exactly as you would see looking through a petrological microscope both in crossed polars and thin section
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