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Rock and Mineral Magnetism

  • W. O’Reilly

Table of contents

  1. Front Matter
    Pages i-xi
  2. W. O’Reilly
    Pages 1-6
  3. W. O’Reilly
    Pages 7-29
  4. W. O’Reilly
    Pages 30-57
  5. W. O’Reilly
    Pages 58-98
  6. W. O’Reilly
    Pages 99-115
  7. W. O’Reilly
    Pages 116-131
  8. W. O’Reilly
    Pages 172-193
  9. W. O’Reilly
    Pages 194-212
  10. Back Matter
    Pages 213-220

About this book

Introduction

The past two decades have witnessed a revolution in the earth sciences. The quantitative, instrument-based measurements and physical models of. geophysics, together with advances in technology, have radically transformed the way in which the Earth, and especially its crust, is described. The study of the magnetism of the rocks of the Earth's crust has played a major part in this transformation. Rocks, or more specifically their constituent magnetic minerals, can be regarded as a measuring instrument provided by nature, which can be employed in the service of the earth sciences. Thus magnetic minerals are a recording magnetometer; a goniometer or protractor, recording the directions of flows, fields and forces; a clock; a recording thermometer; a position recorder; astrain gauge; an instrument for geo­ logical surveying; a tracer in climatology and hydrology; a tool in petrology. No instrument is linear, or free from noise and systematic errors, and the performance of nature's instrument must be assessed and certified. This has been the task of the research worker in rock and mineral magnetism.

Keywords

Pet climatology earth evolution fields geophysics hydrology hysteresis magnetism magnetization mineral noise physics tracer tractor

Authors and affiliations

  • W. O’Reilly
    • 1
  1. 1.University of Newcastle upon TyneUK

Bibliographic information