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Wenji (1986)
Discovery of well-preserved ophiolite on the southeastern margin of the Jiangnan ancient continent and its basic characteristicsActa Petrologica et Mineralogica, 5
D. Wood (1980)
The application of a ThHfTa diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary Volcanic ProvinceEarth and Planetary Science Letters, 50
X. Zhou, J. Yang (1990)
Sm-Nd ISOCHRONOUS AGE OF FUCHUAN OPHIOLITE SUITE IN SHEXIAN COUNTY,ANHUI PROVINCE AND ITS GEOLOGICAL SIGNIFICANCE
J. Pearce (1976)
Statistical Analysis of Major Element Patterns in BasaltsJournal of Petrology, 17
Sibe (1988)
Isotopic ages and geological significance of the pre-Sinian metavolcanic rocks in northeastern JiangxiRegional Geology of China
Abstract Proterozoic rocks in the northeastern Jiangxi‐southern Anhui may fall into three rock associations which belong to different but interrelated tectono‐palaeogeographic units. The field geological and petrochemical characteristics of the northeastern Jiangxi‐western Zhejiang volcanic zone indicate that it was once an island arc zone. An analysis of the sedimentary characteristics of Proterozoic turbidites lying north of the zone has revealed the history of development of a back‐arc basin. According to the type of the Proterozoic rock formation south of the zone, it may be deduced that the formation might represent the fore‐ arc and French areas. By means of various tectono‐palaeogeographic analyses, the relation between the island arc zone and the back‐arc basin is inferred and the Late Proterozoic tectono‐ palaeogeographic development is discussed by using the model of the trench‐arc‐basin system.
Acta Geologica Sinica (English Edition) – Wiley
Published: Sep 1, 1990
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