Abstract
This paper describes the bottom half of a 185 m-long core taken from the Badwater Basin salt pan. Four facies, deposited in a changing saline lacustrine system, appear in the core. The succession of facies is dominated by the development and eventual desiccation of a perennial lake, which was saline during all or most of its long existence. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 61-103 |
| Number of pages | 43 |
| Journal | SEPM Core Workshop |
| Volume | 19 |
| DOIs | |
| State | Published - 1994 |
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