Provenance analysis of the Cretaceous Laiyang Group on Lingshan Island (western Yellow Sea, China) and its tectono-sedimentary implications. Issue 3 (2nd April 2020)

• Record Type: Journal Article
• Authors: Fan, A. P.; Sun, S. N.; Yang, R. C.; Zhang, Z.; De, S.; Nenzhelele, J. D. N.; Li, Y.; Liu, H. P.; Zhou, Y. Q.; Yuan, J.
• Is Part Of: Australian journal of earth sciences. Volume 67:Issue 3(2020)
• Page Start: 361
• Page End: 377
• Publication Date: 2020-04-02
• Subjects: Lingshan Island -- cathodoluminescence -- heavy-mineral analysis -- provenance analysis -- Cretaceous Laiyang Group -- Sulu Orogen; Earth sciences -- Australia -- Periodicals; Earth sciences -- Periodicals; Geology -- Australia -- Periodicals; Geology -- Periodicals; 559.405
• DOI: 10.1080/08120099.2019.1661285
• Languages: English
• ISSNs: 0812-0099

Abstract

Abstract: Longstanding debates on the tectonic setting and provenance of the Lower Cretaceous Lingshandao Formation have hindered basin analysis and tectonic studies of the collision of the Yangtze Craton and the North China Craton, and thus the evolution of the Sulu Orogen. Thin-section analysis, identification of rock particles, cathodoluminescence, heavy minerals and trace-element analysis have, in addition to field investigations, been applied to reconstruct the source area and transport pathways of the sediments that build the Lower Cretaceous Laiyang Group on the Lingshan Island, western Yellow Sea. These analyses indicate that the Laiyang Group consists mainly of material derived from a recycled orogen and from transitional continental sediments. The Laiyang Group on Lingshan Island has been sourced from igneous and metamorphic rocks. Comparing analyses of detrital minerals with rocks from surrounding areas leads to the conclusion that the main source area is the Sulu Orogen that supplied sediment to rift basin rather than a residual basin between the Yangtze Craton and the North China Craton. A recycled orogenic belt is the source area for the Laiyang Group on Linshan Island. Felsic metamorphic and igneous rocks form the most probable sources. The rift basin was filled by sediments supplied from the Sulu Orogen on both sides.