Joint spacing and distribution in deformation band shear zones
Tectonic joints localized within deformation band shear zones on the Kaibab uplift in Utah, USA, show the same spacing and distribution characteristics as joints controlled by primary lithological mechanical stratigraphy, despite the fact that deformation band shear zones are secondary structural fe...
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| Veröffentlicht in: | Geological magazine 2003-01, Vol.140 (1), p.1-9 |
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| container_title | Geological magazine |
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| creator | TINDALL, S. E. DAVIS, G. H. |
| description | Tectonic joints localized within deformation band shear zones on the Kaibab uplift in Utah, USA, show the same spacing and distribution characteristics as joints controlled by primary lithological mechanical stratigraphy, despite the fact that deformation band shear zones are secondary structural features oblique to primary sedimentary layers. The spacing and distribution of joints that traverse deformation band shear zones are important factors in the permeability and connectivity of sandstone reservoirs compartmentalized by deformation band shear zones. |
| doi_str_mv | 10.1017/S0016756802007082 |
| format | Article |
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E.</au><au>DAVIS, G. H.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Joint spacing and distribution in deformation band shear zones</atitle><jtitle>Geological magazine</jtitle><addtitle>Geol. Mag</addtitle><date>2003-01</date><risdate>2003</risdate><volume>140</volume><issue>1</issue><spage>1</spage><epage>9</epage><pages>1-9</pages><issn>0016-7568</issn><eissn>1469-5081</eissn><coden>GEMGA4</coden><abstract>Tectonic joints localized within deformation band shear zones on the Kaibab uplift in Utah, USA, show the same spacing and distribution characteristics as joints controlled by primary lithological mechanical stratigraphy, despite the fact that deformation band shear zones are secondary structural features oblique to primary sedimentary layers. The spacing and distribution of joints that traverse deformation band shear zones are important factors in the permeability and connectivity of sandstone reservoirs compartmentalized by deformation band shear zones.</abstract><cop>Cambridge, UK</cop><pub>Cambridge University Press</pub><doi>10.1017/S0016756802007082</doi><tpages>9</tpages></addata></record> |
| fulltext | fulltext |
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| source | Cambridge Journals |
| subjects | Changes clastic rocks Colorado Plateau connectivity Cretaceous Dakota Formation Deformation faults fractures Geology joints Jurassic Kaibab Formation Kane County Utah Lower Cretaceous Lower Jurassic Mesozoic Navajo Sandstone Paleozoic Permeability Permian planar deformation features Plate tectonics Sandstone sed rocks, sediments Sedimentary petrology sedimentary rocks shear zones Stratigraphy Structural geology style tectonics United States Utah |
| title | Joint spacing and distribution in deformation band shear zones |
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