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Back Matter Source: Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, Vol. 326, No. 1589, Tectonic Evolution of the Himalayas and Tibet (Sep. 1, 1988) Published by: The Royal Society Stable URL: http://www.jstor.org/stable/38126 . Accessed: 01/05/2014 10:59 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. . The Royal Society is collaborating with JSTOR to digitize, preserve and extend access to Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. http://www.jstor.org This content downloaded from 130.132.123.28 on Thu, 1 May 2014 10:59:33 AM All use subject to JSTOR Terms and Conditions

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Page 1: Tectonic Evolution of the Himalayas and Tibet || Back Matter

Back MatterSource: Philosophical Transactions of the Royal Society of London. Series A, Mathematical andPhysical Sciences, Vol. 326, No. 1589, Tectonic Evolution of the Himalayas and Tibet (Sep. 1,1988)Published by: The Royal SocietyStable URL: http://www.jstor.org/stable/38126 .

Accessed: 01/05/2014 10:59

Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at .http://www.jstor.org/page/info/about/policies/terms.jsp

.JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range ofcontent in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new formsof scholarship. For more information about JSTOR, please contact [email protected].

.

The Royal Society is collaborating with JSTOR to digitize, preserve and extend access to PhilosophicalTransactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

http://www.jstor.org

This content downloaded from 130.132.123.28 on Thu, 1 May 2014 10:59:33 AMAll use subject to JSTOR Terms and Conditions

Page 2: Tectonic Evolution of the Himalayas and Tibet || Back Matter

TRACERS IN THE OCEAN

EDITED BY

H. CHARNOCK, F.R.S., J.E. LOVELOCK, F.R.S.,

P.S. LISS AND M. WHITFIELD

Tracer distributions can provide information about the general circulation of the ocean that cannot be obtained in any other way. Modern chemical techniques are providing maps not only of conservative tracers but also of anthropogenically derived transient tracers that are indicative not only of ocean currents but of mixing processes. The sources and sinks and the complicated biological interactions are gradually becoming better understood but the inclusion of tracer data in schemes for the quantitative estimate of ocean currents remains difficult, partly because of our ignorance of the details of mixing processes. These can be directly studied by using purposeful tracers. Particular attention has to be paid to air-sea transfer processes; that of CO2 is crucial to our consideration of climatic change.

This volume, containing papers presented at a meeting on 21 and 22 May 1987, gives an up-to-date account of ocean tracers and their potential, and will be of interest to chemists, geologists and geophysicists as well as to oceanographers and climatologists.

236 pages clothbound ISBN 0 85403 350 5

First published in Philosophical Transactions of the Royal Society, Series A, Vol. 325, 1988

Price including packing and postage

?45.00 (U.K. addresses) ?48.00 (Overseas addresses)

The Royal Society

6 Carlton House Terrace, London, SW1Y 5AG

This content downloaded from 130.132.123.28 on Thu, 1 May 2014 10:59:33 AMAll use subject to JSTOR Terms and Conditions

Page 3: Tectonic Evolution of the Himalayas and Tibet || Back Matter

MAJOR CRUSTAL LINEAMENTS AND

THEIR INFLUENCE ON THE GEOLOGICAL

HISTORY OF THE CONTINENTAL LITHOSPHERE

Crustal lineaments are major faults or fault zones which have ihad a continued influence on the geological evolution of the continental litho- sphere. Contributions to this report evaluate what is known and what is not known about the seismic signatures of major lineaments, their structure and reactivation, their subsequent control of geological processes and their influence on the location of mineral and hydrocarbon deposits.

3 plates clothbound ISBN 0 85403 270 3

First published in Philosophical Transactions of the Royal Society, Series A, Vol. 317, 1986

Price including packing and postage ?45.50 (U.K. addresses) ?48.50 (Overseas addresses)

The Royal Society 6 Carlton House Terrace, London, SW1Y 5AG

Printed in Great Britain for the Royal Society by the University Press, Cambridge

290 pages

This content downloaded from 130.132.123.28 on Thu, 1 May 2014 10:59:33 AMAll use subject to JSTOR Terms and Conditions