Abstract
Cores of organic-rich muds from the tropical meteorite crater Lake Bosumtwi, Ghana, contain laminae of authigenic calcite polyhedra and aragonite needles, as well as scattered diagenetic calcite, Mg-calcite spherulites, and aggregates of dolomite crystals. This example provides a model for the interpetation of ancient lacustrine carbonates from organic-rich environments.-from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 912-916 |
| Number of pages | 5 |
| Journal | Geology |
| Volume | 14 |
| Issue number | 11 |
| DOIs | |
| State | Published - 1986 |
Bibliographical note
Copyright:Copyright 2019 Elsevier B.V., All rights reserved.
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