Biostratigraphy of the tepetate formation Baja California del Sur
Read Online
Share

Biostratigraphy of the tepetate formation Baja California del Sur

  • 568 Want to read
  • ·
  • 47 Currently reading

Published .
Written in English


Book details:

Classifications
LC ClassificationsMicrofilm 69365
The Physical Object
FormatMicroform
Paginationvii, 111 p.
Number of Pages111
ID Numbers
Open LibraryOL1249735M
LC Control Number94895319

Download Biostratigraphy of the tepetate formation Baja California del Sur

PDF EPUB FB2 MOBI RTF

Biostratigraphy of the Tepetate Formation, Baja California del Sur. - Page 86 By OAI identifier: oai::pcoll30/ Nannoplankton biostratigraphy of the Tepetate Formation, Baja California del Sur. - Page 36 By OAI identifier: oai::pcoll30/ The Tepetate formation as an informal lithostrati- graphic unit was named by Heim () to include the marine rocks outcropping near rancho El Tepetate in Arroyo Colorado, Baja California Sur, Mexico. It is constituted by slightly folded, well-strati fi ed sandstone and shale, 1, m thick, and was interpreted as an Eocene neritic deposit. Foraminifera from the Tepetate Formation (Heim) at Las Pocitas, Baja California Sur, Mexico Article (PDF Available) in Ciencias Marinas 34(2) June with Reads How we measure 'reads'.

Baja California is positioned over the well-known San Andreas fault, a rift known for its restlessness responsible for recurrent earthquakes and geologic transformations. Geologists conjecture that the Baja California peninsula was formed million years ago as the fault shifted northward. As such, the peninsula split from mainland Mexico.   To the south, the sequence 3 correlates with the Paleocene–Eocene Bahía Ballenas Formation from the southern part of the Sebastian Vizcaino Peninsula (Abbott et al., ) and the Bateque Formation reported near San Ignacio in southern Baja California (Mina, ; Smith et . An integrated study of Foraminifera, Ostracoda and lithostratigraphy was conducted on samples of the Tepetate Formation from the Arroyo Colorado locality, Baja California Sur (Mexico). Based on the planktonic Foraminifera, Acarinina pentacamerata (latest lower Eocene) and Hantkenina nuttalli (earliest middle Eocene) zones were recognized that. Fossil decapods from the Eocene Tepetate Formation, Baja California Sur, Mexico. Annals of Carnegie Museum, Studi e Ricerche, Associazone Amici del Museo, Museo Civico AG. Zannato, Montecchio Maggiore (Vicenza) Italy, 6 October , p. 21‑ Schweitzer, C. E. and R. M. Feldmann. In Books of Abstracts, Sixth International.

  Baja California Sur’s glorious colonial past has made it a center for historical architecture and traditional art forms, and it’s also a great place to surf and fish. The Tepetate formation as an informal lithostratigraphic unit was named by Heim () to include the marine rocks outcropping near rancho El Tepetate in Arroyo Colorado, Baja California Sur, Mexico. It is constituted by slightly folded, well–stratified sandstone and shale, 1, m thick, and was interpreted as an Eocene neritic deposit. Specimens of calcareous nannoplankton from Las Pocitas core, Tepetate formation, Baja California Sur. All by 2 X. a: Braarudosphaera bigelowii (Gran and Braarud, ) Defl andre, , IGMD Request PDF | On Jan 1, , Gerardo González-Barba and others published Earliest Pacific Basin record of the Pelagornithidae (Aves: Pelecaniformes) | Find, read and cite all the research you.