کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
5483692 | 1522537 | 2016 | 15 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
The origin of lithotype cycles in Oligo-Miocene brown coals from Australia and Germany
ترجمه فارسی عنوان
منشاء چرخه لیتو تیپی در زغال سنگ قهوه ای اولیگو-میوسن از استرالیا و آلمان
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موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی اقتصادی
چکیده انگلیسی
The palaeogeographic setting for Latrobe Valley and German brown coals is similar - in Latrobe Valley the seams split and thin to the east into marine facies. In the Rhenish and Lusatia brown coals they also split and thin to the north into marine facies. The two Rhenish mines at Hambach and Garzweiler respectively typify end members of this palaeogeography - the Hambach mine is located in a distal location where sulphur content is negligible; the Garzweiler mine is located in a proximal location to the marine boundary where sulphur content is higher. The colourimetry and facies succession suggest German brown coal deposition followed a similar cyclic depositional succession to the Latrobe Valley, and that this succession may be fundamental in all thick coal seams.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: International Journal of Coal Geology - Volume 166, 1 September 2016, Pages 47-61
Journal: International Journal of Coal Geology - Volume 166, 1 September 2016, Pages 47-61
نویسندگان
Guy Holdgate, Malcolm Wallace, Matilda O'Connor, Vera Korasidis, Uli Lieven,