| Abstract: | The northern Gulf of Mexico continental shelf is characterized by superimposing deltas. One such delta, informally named Lagniappe, extends east of the Mississippi Delta from mid-shelf to the continental slope. This late Wisconsinan delta is adjacent to, but not associated with the Mississippi Delta complex: the fluvial source was probably the ancient Pearl and/or Mobile Rivers. The fluvially dominated Lagniappe Delta is characterized by complex sigmoid-oblique seismic-reflection patterns, indicating delta switching of high-energy sand-prone facies to low-energy facies. The areal distribution and sediment thickness of the delta were partially controlled by two diapirs. ?? 1989 Springer-Verlag New York Inc. |
| Genre: | Article |
| ProdID: | 70015548 |
| Citation Author: | Kindinger, J. L. |
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| Citation End Page: | 66 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Geo-Marine Letters |
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| Citation Number Of Pages: | 8 |
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| Citation Search Results Text: | Depositional history of the Lagniappe Delta, northern Gulf of Mexico; 1989; Article; Journal; Geo-Marine Letters; Kindinger, J. L. |
| Citation Start Page: | 59 |
| Citation Volume: | 9 |
| Citation Year: | 1989 |
| Type: | citation/reference |
| Text: | Depositional history of the Lagniappe Delta, northern Gulf of Mexico; 1989; Article; Journal; Geo-Marine Letters; Kindinger, J. L. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/10.1007/BF02430425 |
| Date Other: | Sun, 1 Jan 1989 00:00 -0600 |
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