| Abstract: | A 2.2 m thick, Late Eocene (?) dike that intruded the Devonian Buchan Caves Limestone, near Murrindal, Victoria, has produced a narrow contact aureole only centimeters wide in the adjacent host rock. The lack of response of the Buchan Caves Limestone to contact metamorphism is attributed to: 1) prior heating to near 200??C; and 2) the fact that the dike intruded into cool, near surface, low-porosity rocks which may have been in the vadose zone. -from Authors |
| Genre: | Article |
| ProdID: | 70018802 |
| Citation Author: | Barker, C. E.; Bone, Y. |
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| Citation End Page: | 164 |
| Citation Issue: | 1 |
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| Citation Language: | English |
| Citation Larger Work Title: | Organic Geochemistry |
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| Citation Number Of Pages: | 14 |
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| Citation Search Results Text: | The minimal response to contact metamorphism by the Devonian Buchan Caves Limestone, Buchan Rift, Victoria, Australia; 1995; Article; Journal; Organic Geochemistry; Barker, C. E.; Bone, Y. |
| Citation Start Page: | 151 |
| Citation Volume: | 22 |
| Citation Year: | 1995 |
| Type: | citation/reference |
| Text: | The minimal response to contact metamorphism by the Devonian Buchan Caves Limestone, Buchan Rift, Victoria, Australia; 1995; Article; Journal; Organic Geochemistry; Barker, C. E.; Bone, Y. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sun, 1 Jan 1995 00:00 -0600 |
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