GS SP 176 - Deformation of Glacial Materials

A. J. Maltman, B. Hubbard, and M. J. Hambrey


$114.00
Member Price
$190.00
Nonmember Price
Buy Now

 

The flow of glacier ice can produce structures that are striking and beautiful. Associated sediments, too, can develop spectacular deformation structures, and examples are remarkably well preserved in Quaternary deposits. Although such features have long been recognized, they are now the subject of new attention from glaciologists and glacial geologists.

This collection of papers addresses how the methods for unravelling deformation structures evolved in recent years by structural geologists can be used for glacial materials, and the opportunities offered to structural geologists by glacial materials for studying deformation in rocks. There are authoritative reviews by leading scientists with a global coverage.

Geological Society of London Special Publication 176

European customers, please order direct from the Geological Society, +44-(0)1225-445046.
Product Code:222
Publisher:Geological Society of London
Release Date:
ISBN:186239072X
Media:Hardback
Pages:

Comments (0)

 

See Also: Field Seminar

Field Seminar In Conjunction with AAPG Annual Convention & Exhibition (ACE) — Canadian Society of Petroleum Geologists (CSPG) ACE FT 13 | The Mid-Paleozoic Exshaw/Banff Unconventional Petroleum System, Alberta: Correlative of Bakken Tight-Oil Play in Williston Basin ACE FT 13 | The Mid-Paleozoic Exshaw/Banff Unconventional Petroleum System, Alberta: Correlative of Bakken Tight-Oil Play in Williston Basin Desktop /Portals/0/PackFlashItemImages/WebReady/Field Trip 13 - CSPG The Mid-Paleozoic Exshaw.jpg?width=100&h=100&mode=crop&anchor=middlecenter&quality=75amp;encoder=freeimage&progressive=true 23972

See Also: Online Certificate Course

Online Certificate Course Geothermal Energy Basics: A Renewable Energy Certificate Course Geothermal Energy Basics: A Renewable Energy Certificate Course Desktop /Portals/0/PackFlashItemImages/WebReady/oc-cc-geothermal-energy-basics.jpg?width=100&h=100&mode=crop&anchor=middlecenter&quality=75amp;encoder=freeimage&progressive=true 433