عرض عادي

The evolution of North America / by Philip B. King.

بواسطة:نوع المادة : نصنصالناشر:Princeton, New Jersey : Princeton University Press, 1977وصف:xv, 197 pages : illustrations, maps ; 29 cmنوع المحتوى:
  • text
نوع الوسائط:
  • unmediated
نوع الناقل:
  • volume
تدمك:
  • 0691081956
  • 9780691081953
  • 069102359X
  • 9780691023595
  • 0691079609
  • 9780691079608
  • 9780691603674
  • 0691603677
الموضوع:تصنيف مكتبة الكونجرس:
  • QE71 .K54 1977
المحتويات:
The natural history of continents -- The Canadian Shield and its ancient rocks -- The Interior Lowlands and the science of genrly-dipping strata -- Appalachian and related systems; Paleozoic structures southeast and south of Central Stable Region -- Lands and seas south of the continent: modern analogues of geosynclines -- The mountain belt of western North America; introduction to the Cordilleran system -- The Eastern Ranges and Plateaus; a novel structural element -- The main part of the Cordillera: its geosyncline and the mountain belt that formed from it -- Cenozoic rocks and structures of the main part of the Cordillera; later modifications of the fundamental structure.
المقتنيات
نوع المادة المكتبة الحالية رقم الطلب رقم النسخة حالة تاريخ الإستحقاق الباركود
كتاب كتاب UAE Federation Library | مكتبة اتحاد الإمارات General Collection | المجموعات العامة QE71 .K54 1977 (إستعراض الرف(يفتح أدناه)) C.1 Library Use Only | داخل المكتبة فقط 30020000040662

Princeton Legacy Library.

Includes bibliographical references and index.

The natural history of continents -- The Canadian Shield and its ancient rocks -- The Interior Lowlands and the science of genrly-dipping strata -- Appalachian and related systems; Paleozoic structures southeast and south of Central Stable Region -- Lands and seas south of the continent: modern analogues of geosynclines -- The mountain belt of western North America; introduction to the Cordilleran system -- The Eastern Ranges and Plateaus; a novel structural element -- The main part of the Cordillera: its geosyncline and the mountain belt that formed from it -- Cenozoic rocks and structures of the main part of the Cordillera; later modifications of the fundamental structure.

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