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▪ extensional tectonics research -- global and australian margin.
:: بحوث الامتداد التكتوني - عالميا وفي الحافة الأسترالية.
Ultimo aggiornamento 2016-12-02
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in, extensional tectonics and stratigraphy of the north atlantic margins.
in, extensional tectonics and stratigraphy of the north atlantic margins.
Ultimo aggiornamento 2013-02-19
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in imaging, mapping and modelling extensional processes and systems, geological society of london special publication, 282.
in imaging, mapping and modelling extensional processes and systems, geological society of london special publication, 282.
Ultimo aggiornamento 2016-12-02
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*dickinson, william r. "the basin and range province as a composite extensional domain".
* dickinson, william r. "the basin and range province as a composite extensional domain".
Ultimo aggiornamento 2016-03-03
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gac/mac meeting on extensional tectonics and stratigraphy of the north atlantic margins, st. john's, newfoundland, may 1988
اجتماع الجمعية الجيولوجية الكندية وجمعية علوم المعادن الكندية (gac/mac) بشأن التحركات اﻻمتدادية للقشرة اﻷرضية ووصف الطبقات اﻷرضيــة لحــواف شمــال اﻷطلسـي، سانــت جونــز، نيو فاوندلند، أيار/مايو ١٩٨٨
Ultimo aggiornamento 2016-12-01
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(b) rifted (extensional, passive) continental margins were formed along incipient plate boundaries during continental breakup and subsequent initial production of oceanic crust by sea-floor spreading (e.g. bally, 1988; edwards and santogrossi, 1990; von rad et al., 1982; coffin and eldholm, 1991). the category of rifted continental margins can be subdivided into two types:
)ب( الحواف القارية )اﻻمتدادية، السلبية( المتصدعة التي تشكلت على طول الحدود اﻷولية للصفيحة القارية أثناء التكسر القاري وما تﻻه من نشوء للقشرة المحيطية الناتج من انتشار قاع البحار. )على سبيل المثال، bally, 1998; edwards and santogrossi, 1990; von rad et al., 1982; coffin and eldholim, 1991( ويمكن تقسيم فئة الحواف القارية المتصدعة إلى نوعين:
Ultimo aggiornamento 2016-12-01
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