caa a22 4500 445301074 CHVBK 20180317142558.0 cr unu---uuuuu 170323e20100201xx s 000 0 eng 10.1007/s11430-010-0010-6 doi (NATIONALLICENCE)springer-10.1007/s11430-010-0010-6 Early diagenetic deformation structures of the Furongian ribbon rocks in Shandong Province of China—A new perspective of the genesis of limestone conglomerates [Elektronische Daten] [JiTao Chen, ZuoZhen Han, XiaoLei Zhang, AiPing Fan, RenChao Yang] Ribbon rocks are characterized by an alternation of millimeter- to centimeter-thick limestone and argillaceous deposits (marlstone or shale). The sedimentary processes and diagenetic characteristics of ribbon rocks might be critical to the formation of limestone conglomerates. According to detailed field measurement and laboratory analyses (thin section observation and XRD analysis), four types of ribbon rocks are classified, i.e., limestone and marlstone couplet (L-M), limestone and shale couplet (L-S), thin-bedded lime mudstone (Ltb), and laminated limestone and marlstone couplet (Cl). These ribbon rocks were mostly deposited in low-energy subtidal environments (below fair-weather wave base). Ribbon rocks exhibit various subtle deformation structures such as intrastratal cracks and "boudin” structures. Differential cementation of carbonate and argillaceous layers during early diagenesis is a prerequisite condition for the deformation of ribbon rock under compaction. Ribbon rocks would be deformed into limestone conglomerates under differential compaction that might be triggered by external forces such as storm and earthquake. Science in China Press and Springer Berlin Heidelberg, 2010 ribbon rock nationallicence cracks nationallicence "boudin” structure nationallicence early diagenesis nationallicence pseudoconglomerate nationallicence Furongian nationallicence Shandong Province nationallicence Chen JiTao College of Geological Science and Engineering, Shandong University of Science and Technology, 266510, Qingdao, China aut Han ZuoZhen College of Geological Science and Engineering, Shandong University of Science and Technology, 266510, Qingdao, China aut Zhang XiaoLei College of Geological Science and Engineering, Shandong University of Science and Technology, 266510, Qingdao, China aut Fan AiPing College of Geological Science and Engineering, Shandong University of Science and Technology, 266510, Qingdao, China aut Yang RenChao College of Geological Science and Engineering, Shandong University of Science and Technology, 266510, Qingdao, China aut Science China Earth Sciences SP Science in China Press 53/2(2010-02-01), 241-252 1674-7313 53:2<241 2010 53 11430 https://doi.org/10.1007/s11430-010-0010-6 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/s11430-010-0010-6 text/html Onlinezugriff via DOI NATIONALLICENCE 700 1- Chen JiTao College of Geological Science and Engineering, Shandong University of Science and Technology, 266510, Qingdao, China aut NATIONALLICENCE 700 1- Han ZuoZhen College of Geological Science and Engineering, Shandong University of Science and Technology, 266510, Qingdao, China aut NATIONALLICENCE 700 1- Zhang XiaoLei College of Geological Science and Engineering, Shandong University of Science and Technology, 266510, Qingdao, China aut NATIONALLICENCE 700 1- Fan AiPing College of Geological Science and Engineering, Shandong University of Science and Technology, 266510, Qingdao, China aut NATIONALLICENCE 700 1- Yang RenChao College of Geological Science and Engineering, Shandong University of Science and Technology, 266510, Qingdao, China aut NATIONALLICENCE 773 0- Science China Earth Sciences SP Science in China Press 53/2(2010-02-01), 241-252 1674-7313 53:2<241 2010 53 11430 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer