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| | Geophysical Corner (AAPG Expl, 11/99) |
 | | The basement fractures are reactivated at later times during, or after, deposition of the sedimentary section and create structures and/or sedimentary facies that become oil and gas traps and reservoirs. |
 | | Shear zones in the basement are one, two or three kilometers in width, are characterized by crushed and broken rock across the entire width, and are usually steeply dipping. |
 | | However, the lithology of the basement is the primary influence on magnetic maps, and structure is a secondary, and sometimes insignificant, factor. |
| www.aapg.org /explorer/geophysical_corner/1999/gpc11.cfm (1100 words) |
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