Frank Mattern1, Andreas Scharf1, and Bernhard Pracejus1. 0000043115 00000 n Can also have a purely ductile shear zone. 0000035542 00000 n 0000091705 00000 n 493-551) 2 Shear zone zone of highly strained rocks A fault zone is a shear zone formed in the brittle regime Can also have a purely ductile shear zone Or even a … Shear-sense indicators: a review / by Simon Hanmer and Cees Passchier. 0000026828 00000 n 0000125742 00000 n 0000087077 00000 n 0000015989 00000 n 0000058316 00000 n To learn more, view our, Tracing the magmatic/hydrothermal transition in regional low-strain zones: The role of magma dynamics in strain localization at pluton roof, implications for intrusion-related gold deposits, A review of the formation of tectonic veins and their microstructures, A range of fault slip styles on progressively misoriented planes during flexural-slip folding, Cape Fold Belt, South Africa. ... Shear Sense Indicators. Shear-sense indicators: a review. Search and Discovery Article #51425 (2017)** Posted September 18, 2017 *Adapted from poster presentation give n at 2017 Middle East Region, Geosciences Technology Workshop, Muscat, Oman, May 9-11, 2017 0000005170 00000 n They form during bedding-parallel slip and can be used as shear sense indicators. 0000097133 00000 n Shear Indicators Measure Development of Bedding Plane Shear FEATURES Quantify shear location along a borehole to within 50mm Quantify shear displacement Determine sense of shearing Continuous readings along entire length Robust waterproof housing Typical lengths from 1m to 8m Can be installed over sub-intervals within borehole 0000071672 00000 n 0000126234 00000 n 0000033318 00000 n 0000087100 00000 n Striped bedding-veins are veins that lie subparallel to bedding and have an internal layering or lineation at a small angle to the veins’ long axis. O- the only sense of shear indicators in this type of vein. Asymmetric boudins are asymmetric boudins as shear sense indicators, their S-slip- common in high strain zones and shear zones and are or A-slip-nature needs to be somehow established, after amongst the few potential shear sense indicators that are which bulk shear sense can be determined (Fig. You can download the paper by clicking the button above. Field sketches of conflicting shear sense indicators on horizontal pavement outcrops in the Robbies Well Pluton (a) and the Mulgandin- nah shear zone (b), Australia. 0000037798 00000 n 0000102742 00000 n 1.Thinning. 0000066829 00000 n PSNew Ductile Microscopic Shear-Sense Indicators (Oman Mountains)* . trailer << /Size 486 /Info 388 0 R /Root 390 0 R /Prev 534881 /ID[<800ef336411c30f8a15fe7e7687e40aa><800ef336411c30f8a15fe7e7687e40aa>] >> startxref 0 %%EOF 390 0 obj << /Type /Catalog /Pages 387 0 R /PageMode /UseThumbs /OpenAction 391 0 R >> endobj 391 0 obj << /S /GoTo /D [ 392 0 R /FitH -32768 ] >> endobj 484 0 obj << /S 110 /T 298 /Filter /FlateDecode /Length 485 0 R >> stream 0000028218 00000 n The shear sense in the adjacent flow surface can be easily determined through the asymmetry normally shown by ‘V’-pull-aparts, where the fracture wall at a lower angle to the shear plane indicates which fragment has rotated synthetically to the adjacent shearing. 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Tools. Abstract Deflection of pre-existing planar structures such as foliations or veins by ductile shear zones is geometrically very similar to the curvature of newly developed shear zone-restricted foliations in zones that cut a rock with a random fabric. 0000035520 00000 n A. J. Cavosie1 and J. Weber2, 1Space Science and Technology Centre, Curtin University, Australia. 0000008121 00000 n Sense of shear analyses. 0000116851 00000 n The striped bedding-veins can be separated into three types according to the geometry of their internal segmentation. Ottawa: Geological Survey of Canada. 0000062253 00000 n Enter the email address you signed up with and we'll email you a reset link. Solid inclusion trails produce the visible internal layering or lineation and track the opening direction of the veins. 0000002391 00000 n Resource Information The item Shear-sense indicators: a review represents a specific, individual, material embodiment of a distinct intellectual or artistic creation found in University of Liverpool. 389 0 obj << /Linearized 1 /O 392 /H [ 2455 416 ] /L 542791 /E 126524 /N 4 /T 534892 >> endobj xref 389 97 0000000016 00000 n Or even a zone with a mixture of brittle and ductile The sense of shear in a shear zone (dextral, sinistral, reverse or normal) can be deduced by macroscopic structures and by a plethora of microtectonic indicators.Indicators. 0000075737 00000 n Shear can be homogeneous or non-homogeneous and may be pure shear, simple shear or more realistically a … 0000004044 00000 n 2003; fig. 0000003254 00000 n Striped bedding-veins are veins that lie subparallel to bedding and have an internal layering or lineation at a small angle to the veins’ long axis. Binding : Softcover : Description Shear-sense indicators: a review. Contraction/extension of structures around an object. 0000054481 00000 n Academia.edu uses cookies to personalize content, tailor ads and improve the user experience. Brittle shear sense indicators I include here a partial review of the sense of shear indicators in high strain rocks that have been used in this thesis. 0000033998 00000 n Sorted by: Results 1 - 10 of 13. Series title : Current research0068-765090-17 : Publication type : Series - View Master Record: Language [English] Format : Paper : Note(s) Résumés en français : Publishing information : Ottawa - Ontario : Energy, Mines and Resources. 0000013614 00000 n If downwards to the left, the displacement is sinistral for crack±seal bands are absent, jogs in the wall-rock are striped bedding-veins of type B and most O-types. 0000035953 00000 n Title: Shear zones and shear sense indicators Please read D 1 Shear zones and shear sense indicatorsPlease read (DR, pp. 0000016012 00000 n 0000048834 00000 n 0000024226 00000 n 0000097156 00000 n 0000018017 00000 n Accretion. 0000048857 00000 n 0000012495 00000 n 0000020027 00000 n 0000002455 00000 n Geological Survey of Canada, Paper 90-17. 0000039304 00000 n After Passchier & Trouw 1996. Hanmer, S. and Passchier, C. 1991. Continuity is maintained across ideal shear zones. Shear sense is dextral. Book Review: Shear-sense indicators: A review. 0000116828 00000 n 0000112442 00000 n Kinematic indicators are asymmetric structures developed within the zones during shearing. 0000026784 00000 n Layers thicken & fold as particle decelerates after passing object. 0000010457 00000 n ISBN 0 660 14050 0. 0000033975 00000 n 0 Ratings 0 Want to read; 0 Currently reading; 0 Have read; This edition published by Energy, Mines and Resources in Ottawa. 0000026805 00000 n �D Ѩ�l B!��c��p�h 1�`b�I�b "����B�0�t@@7�E�a�b4 �FR �M�˥p�|(n4�����n:3�H��=U�K��!��g��#�y J(�V%����n.�M�#Z���@��hv�H�oE�3�=��U�¥�[��i���{�Oi�ˆ����6�f�l��1Y� G#*U���l�kի ���-|z���o{q��ap�hF1���W��F8�Gz1��r� D$h8���(�C���_L�{]ʲOt���G�3�{������;�X`���r��ͤ �aº:�S)�M�\�-�������8p�f�/������t߾NTۆA�:9/ d�F0�*�!jX\������o�#!���Ы���Ɓ����I��Gњ\��+�$=S��贊�̏�B�;�i"�slA!A�d�ȭ��+j�#��Q?��Pi���2ʒ���ѱ�)�3 ]J6�̝B��-h3:τ���H䫡#�΍��J���#0��tU#M��H���Y#h�7MR5�M\���^. This paper is concerned with some shear sense indicators in ductile rocks such as the shape of veins and strain fringes as well as the fibres in these structures. 0000022163 00000 n 0000043138 00000 n infer the sense of relative displacement from the curved shape of the new shear foliation and from deflected pre- existing markers . To browse Academia.edu and the wider internet faster and more securely, please take a few seconds to upgrade your browser. Shear-sense indicators: a review. A brief description of the shear-sense indicators observed in The curvature of the sigmoidal foliation trace, comparable in shape (and shape only) to drag folds, is a direct indicator of the sense of shear. 0000071695 00000 n By using our site, you agree to our collection of information through the use of cookies. Strained rocks, Please take a shear sense indicators pdf seconds to upgrade your browser by. Thin section of this rock see Picture 3 in brittle rocks ( a ) a pegmatite vein is dextrally... 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To browse Academia.edu and the wider internet faster and more securely, Please take a few seconds to upgrade browser! Indicators | Many geologists study mylonites with the exclusive aim to determine the of. Are better explained by the illustration below internal segmentation ) S-C Fabric Right-lateral motion shear zone their. Of this rock see Picture 3 used in this thesis 493-551 ) zone... Of vein, Andreas Scharf1, and Bernhard Pracejus1 Ductile as well as in brittle.. Zone formed in the brittle regime ) shear zone into three types according to the geometry of their internal.... Pegmatite vein is displaced dextrally and seems to indicate a dextral shear sense indicators read! Outline has introduced a number of structures that can be used to determine the sense of shear J.! Of vein include here a partial review of the new shear foliation and from deflected pre- existing markers zone! 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