کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4696295 | 1351665 | 2009 | 5 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Glacioeustatic sea level fall marking the base of supercycle TA-1 at 66.5Â Ma recorded by the kaolinization of the Whitemud Formation and the Colgate Member of the Fox Hills Formation
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موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی اقتصادی
پیش نمایش صفحه اول مقاله
![عکس صفحه اول مقاله: Glacioeustatic sea level fall marking the base of supercycle TA-1 at 66.5Â Ma recorded by the kaolinization of the Whitemud Formation and the Colgate Member of the Fox Hills Formation Glacioeustatic sea level fall marking the base of supercycle TA-1 at 66.5Â Ma recorded by the kaolinization of the Whitemud Formation and the Colgate Member of the Fox Hills Formation](/preview/png/4696295.png)
چکیده انگلیسی
The Colgate Member of the Fox Hills Formation in Montana is an exact correlative of the Whitemud, and kaolinization of the Colgate is due to the same sea level fall from the International Boundary to central North Dakota. The age correlates to the sea level cycle marking the base of supercycle TA-1, and the short duration indicates that this sea level cycle was glacioeustatic.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Marine and Petroleum Geology - Volume 26, Issue 7, August 2009, Pages 1299-1303
Journal: Marine and Petroleum Geology - Volume 26, Issue 7, August 2009, Pages 1299-1303
نویسندگان
J.F. Lerbekmo,