Hydrothermal pebble dikes at Mount Morgan, Queensland

Cornelius K.D. (1967) Hydrothermal pebble dikes at Mount Morgan, Queensland. Economic Geology, 62 6: 853-860. doi:10.2113/gsecongeo.62.6.853

Author Cornelius K.D.
Title Hydrothermal pebble dikes at Mount Morgan, Queensland
Journal name Economic Geology   Check publisher's open access policy
ISSN 0361-0128
Publication date 1967-09-01
Sub-type Article (original research)
DOI 10.2113/gsecongeo.62.6.853
Open Access Status Not yet assessed
Volume 62
Issue 6
Start page 853
End page 860
Total pages 8
Publisher Society of Economic Geologists
Subject 1906 Geochemistry and Petrology
1908 Geophysics
1905 Visual Arts and Crafts
1907 Geology
Abstract Dikes are mostly 1-2 feet thick, with sharp contacts and no wall-rock alteration. Matrix of clay- to sand-size particles makes up 50-70 percent of volume. Fragments show a wide range in degree of rounding and include fragments of granite from at least 1500 feet below exposures. Emplacement is attributed to fluidization by hydrothermal liquid.
Q-Index Code C1
Q-Index Status Provisional Code
Institutional Status Unknown

Document type: Journal Article
Sub-type: Article (original research)
Collection: Scopus Import - Archived
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Citation counts: Scopus Citation Count Cited 2 times in Scopus Article | Citations
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Created: Tue, 14 Jun 2016, 10:27:10 EST by System User