Lyell Collection

Geological Society, London, Special Publications

Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help


Keywords:
Author:
Advanced search>>
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Cronin, V. S.
Right arrow Articles by Sverdrup, K. A.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Geological Society, London, Special Publications; 1993; v. 74; p. 193-206;
DOI: 10.1144/GSL.SP.1993.074.01.14
© 1993 Geological Society of London

North and West Pakistan

Preliminary Landsat lineament analysis of the northern Nanga Parbat-Haramosh Massif, northwest Himalaya

V. S. Cronin1, G. J. Schurter1,2 & K. A. Sverdrup1

1 Geosciences Department, University of Wisconsin-Milwaukee, PO Box 413, Milwaukee, Wisconsin 53201, USA
2 Amoco Production Company, PO Box 3092, Houston, Texas 77253, USA

Analysis of a mosaic of Landsat 2 MSS band 7 images covering the northern Nanga Parbat-Haramosh Massif (NPHM) has yielded approximately 540 lineaments, defined by sets of colinear drainage segments and aligned linear graytone boundaries. We recognized segments of the few well-mapped faults along the NPHM as lineaments. The paucity of field data concerning faults, joints, lithological fabric and contacts prevents us from interpreting most of the lineaments at this time. However, some of the prominent lineament trends probably mark the trace of previously unmapped active faults that accommodate the recent uplift of the NPHM. The origins of these lineaments must be established through structural geological field work.