| Abstract: | Tectonic processes associated with subduction of oceanic crust, but unrelated to the collision of thick crustal masses or microplates, are presumed by many geologists to significantly affect the formation and deformation of large sedimentary bodies at underthrust ocean margins. More geologists are familiar with the concept of subduction accretion than with other noncollision processes - for example, sediment subduction, subduction erosion, and subduction kneading. In our opinion, no single subduction-related tectonic process is the dominant or typical one that forges the geologic framework of modern underthrust ocean margins. It is likely, therefore, that the rock records of ancient underthrust margins are preserved in a multitude of structural and stratigraphic forms.-from Authors |
| Genre: | Article |
| ProdID: | 70012272 |
| Citation Author: | Scholl, D. W.; Von Huene, R.; Vallier, T. L.; Howell, D. G. |
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| Citation End Page: | 568 |
| Citation Issue: | 12 |
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| Citation Language: | English |
| Citation Larger Work Title: | Geology |
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| Citation Number Of Pages: | 5 |
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| Citation Search Results Text: | Sedimentary masses and concepts about tectonic processes at underthrust ocean margins ( subduction).; 1980; Article; Journal; Geology; Scholl, D. W.; Von Huene, R.; Vallier, T. L.; Howell, D. G. |
| Citation Start Page: | 564 |
| Citation Volume: | 8 |
| Citation Year: | 1980 |
| Type: | citation/reference |
| Text: | Sedimentary masses and concepts about tectonic processes at underthrust ocean margins ( subduction).; 1980; Article; Journal; Geology; Scholl, D. W.; Von Huene, R.; Vallier, T. L.; Howell, D. G. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Tue, 1 Jan 1980 00:00 -0600 |
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