About This Item
- Full TextFull Text(subscription required)
- Pay-Per-View PurchasePay-Per-View
Purchase Options Explain
Share This Item
The AAPG/Datapages Combined Publications Database
AAPG Bulletin
Abstract
Volume:
Issue:
First Page:
Last Page:
Title:
Author(s):
Abstract:
The relationships of the Permian formations exposed in the Guadalupe, Delaware, and Apache mountains and immediately east have for some time been the subject of much dispute. These are greatly clarified by the classification of the Capitan and Apache limestones as reef formations built on the flanks of a large, subsiding basin. This basin was formed principally after the deposition of the lower Delaware limestone and then was partly filled with Delaware sand. The reefs were built during the deposition of the upper part of the Delaware sandstones. The Carlsbad limestones are considered the lagoonal facies of the reef series.
After being restricted from open marine conditions, the basin was filled with the products of an evaporating sea, the Castile gypsum and a distinct salt series.
No attempt is made to subdivide Darton's Chupadera in other parts of New Mexico.
Pay-Per-View Purchase Options
The article is available through a document delivery service. Explain these Purchase Options.
| Watermarked PDF Document: $14 | |
| Open PDF Document: $24 |
AAPG Member?
Please login with your Member username and password.
Members of AAPG receive access to the full AAPG Bulletin Archives as part of their membership. For more information, contact the AAPG Membership Department at [email protected].