کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
8914583 | 1640633 | 2018 | 9 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
The stratigraphy and origin of the Tofts ridge in north-western Fenland, eastern England
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی
پیش نمایش صفحه اول مقاله
![عکس صفحه اول مقاله: The stratigraphy and origin of the Tofts ridge in north-western Fenland, eastern England The stratigraphy and origin of the Tofts ridge in north-western Fenland, eastern England](/preview/png/8914583.png)
چکیده انگلیسی
The Tofts located in north-western Fenland is a low ridge composed of sandy silt, elevated several metres above the surrounding land. Stratigraphically, the feature is the landward edge of an intertidal-subtidal sand body that stretches east into The Wash. It was the location of a Medieval salt-making industry. The ridge seems to have been initiated after 2100â¯calâyears BP by storm waves and/or wind transporting sediment landward from adjacent intertidal flats. Differential consolidation of peat on its landward side and dumping of sediment onto the surface during salt-making enhanced its morphological expression.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Proceedings of the Geologists' Association - Volume 129, Issue 2, April 2018, Pages 135-143
Journal: Proceedings of the Geologists' Association - Volume 129, Issue 2, April 2018, Pages 135-143
نویسندگان
David S. Brew, Graham Evans,