新墨西哥州中西部晚白垩纪(塞诺曼尼亚)Seboyeta湾向西延伸

Mogollon Slope (West-Central New Mexico and East-Central Arizona) Pub Date : 1900-01-01 DOI:10.56577/ffc-45.255

O. J. Anderson, S. Lucas

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引用次数: 1

摘要

—在卡特龙县最西部沿Cottonwood峡谷的达科他砂岩上部存在以Exogyra levis Stephenson和Granocardium enstromi (Bergquist)为主的软体动物化石组合。这些化石与达科他砂岩的中Cenomanian pagate舌具有相关性。因此，它们将帕格特沉积的塞博耶塔湾向西南偏西延伸40公里。

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Westward extension of Seboyeta Bay, late Cretaceous (Cenomanian) of west-central New Mexico

-A molluscan fossil assemblage dominated by Exogyra levis Stephenson and Granocardium enstromi (Bergquist) is present in the upper part of the Dakota Sandstone along Cottonwood Canyon in extreme western Catron County. These fossils indicate correlation with the middle Cenomanian Paguate Tongue of the Dakota Sandstone. They thus extend the Seboyeta bay in which the Paguate was deposited 40 km to the west-southwest.

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Mogollon Slope (West-Central New Mexico and East-Central Arizona)

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