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Origin of Granite Batholiths Geochemical Evidence: Based on a meeting of the Geochemistry Group of the Mineralogical Society
Atherton Tarney(Eds)
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Description for Origin of Granite Batholiths Geochemical Evidence: Based on a meeting of the Geochemistry Group of the Mineralogical Society
paperback. Num Pages: black & white illustrations, bibliography. BIC Classification: RBG; WNR. Category: (G) General (US: Trade). Dimension: 229 x 152 x 9. Weight in Grams: 222.
This book is for undergraduates, postgraduates and research workers who wish to gain an insight into present ideas and speculations on the origin of granite batholiths. It is a summary of the proceedings of a one-day meeting of the Geochemistry Group of the Mineralogical Society held at the University of liverpool on the 2nd May 1979, entitled The Origin of Granite Batholiths: Geochemical Evidence. It was felt that relevant new geochemical and isotopic data with associated field and petrological observations would be helpful in clarifying the main issues connected with the origin of granitic rocks. The speakers who participated contri ... Read more
This book is for undergraduates, postgraduates and research workers who wish to gain an insight into present ideas and speculations on the origin of granite batholiths. It is a summary of the proceedings of a one-day meeting of the Geochemistry Group of the Mineralogical Society held at the University of liverpool on the 2nd May 1979, entitled The Origin of Granite Batholiths: Geochemical Evidence. It was felt that relevant new geochemical and isotopic data with associated field and petrological observations would be helpful in clarifying the main issues connected with the origin of granitic rocks. The speakers who participated contri ... Read more
Product Details
Format
Paperback
Publication date
2012
Publisher
Birkhäuser United States
Condition
New
Number of Pages
148
Place of Publication
New York, United States
ISBN
9781468479904
SKU
V9781468479904
Shipping Time
Usually ships in 15 to 20 working days
Ref
99-15
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