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Geochemical Indication of Sinian Bedded Siliceous Rocks in the Hunan‐Guizhou‐Guangxi Area and Their Environmental Significance
Author(s) -
Jim PENG,
Haisheng YI,
Wenjie XIA
Publication year - 2000
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/j.1755-6724.2000.tb00430.x
Subject(s) - geology , hydrothermal circulation , sedimentary depositional environment , geochemistry , sedimentary rock , mineralogy , structural basin , geomorphology , paleontology
In the Hunan‐Guizhou‐Guangxi area there have developed very thick bedded siliceous rocks of the late Sinian. The rocks have a fairly pure composition, with an average content of siliceous minerals exceeding 95%. They are relatively rich in Fe and Mn, and poor in Al, Ti and Mg. The Fe/Ti, (Fe+Mn)/Ti, Al/(Al+Fe+Mn) and U/Th ratios and the Al‐Fe‐Mn and Fe‐Mn‐(Ni+Co+Cu)×10 triangle diagrams all show that they are hydrothermal sedimentary siliceous rocks. In the rocks the total amount of REEs is low, the δCe shows an obvious negative anomaly and the δEu a weak anomaly, and LREE>HREE, all indicating that they are products of hydrothermal processes. The δ 30 Si and δ 18 O values, as well as the formation temperature of the rocks all clearly show that the silica forming the rocks comes from hot water. Besides, analyses of the depositional environment of the rocks using the MnO/TiO 2 ratio and the δCe and δ 30 Si values yield the same conclusion that they are formed in environments from continental marginal slopes of a bathyal environment to oceanic basins of a deep‐sea environment.