Siliceous rock in strata: research progress and prospect
ZHOU Siyu1,2, ZHONG Dakang1,2, SUN Haitao1,2, ZHANG Benjian3, SU Chen3, YIN Hong4
1 College of Geosciences,China University of Petroleum(Beijing),Beijing 102249,China; 2 State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum(Beijing),Beijing 102249,China; 3 Exploration and Development Research Institute of PetroChina Southwest Oil and Gas Field Company,Chengdu 610041,China; 4 Northwest Sichuan Gas Field,Southwest Oil and Gasfield Company,PetroChina,Sichuan Jiangyou 621700,China
Abstract：Siliceous rocks are a chemical sedimentary rock formed from authigenic quartz,usually in layered or non-layered(condullary,banded)forms,either alone,interbedded,and in other lithologic Formations. Silica not only records a large amount of geological information of the basin's paleogeography,paleo-ocean and paleoclimate,but also plays an important role in the study of rock geotectonics. The previous research on siliceous rocks has achieved rich results. In recent years,new viewpoints on siliceous rocks have provided new ways of understanding and research clues for the study of siliceous rocks. By investigating the petrological characteristics,geochemical characteristics and sedimentary environment of siliceous rocks in recent years,this paper analyzes and summarizes the Formation modes,genetic types and discrimination methods of siliceous rocks in different geological historical periods,different depositional environments,and different occurrences. The sedimentation of siliceous rocks is not the result of single factor control,but the comprehensive result of geological tectonic activity intensity,biological type and activity,and sedimentary paleoenvironments. Conventional geochemical elements,combined with rock fabric and micro-area analysis,inclusion analysis,new isotope(Rb-Sr and Sm-Nd)analysis,and new geochemical criteria(Ge/Si)are an essential methodology for silica research and method.
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