安徽南部下二叠统结核状硅质岩和层状硅质岩的沉积学特征及其成因探讨

Sedimentological Features and the Genesis of Lower Permian Nodular and Thin-Bedded Siliceous Rocks in Southern Anhui

前言根据岩性特征和生物化石组合带,安徽南部下二叠统可划分为栖霞组和孤峰组。栖霞组主要为一套含硅质结核及硅质条带的灰岩建造。灰岩中含大量的藻类、(虫廷)、有孔虫、珊瑚、腕足和棘皮等浅海底栖型生物化石。孤峰组主要为一套薄层状硅质岩与薄层状泥页岩互层,组成硅—泥韵律沉积建造,含薄壳腕足、菊石、小有孔虫、硅质海绵和放射虫等浮游型生物化石。据两条主干部面(巢湖龟山、宿松坐山)统计,下二叠统碳酸盐岩占地层总厚的81.2％,

Based on rock types and fossil assemblages, the Qixia and Gufeng Formations may be distinguished for the Lower Permian in southern Anhui. The Qixia Formation is composed dominantly of a suite of nodular and striped siliceous limestones which contain abundant neritic benthonic organisms such as algae, fusulinids, benthonic foraminifera, corals, brachiopods, echinoderms and bryozoa. The Gufeng Formation is dominated by a suite of sedimentary sequences consisting of thin-bedded siliceous rock/muddy shale couplets which comprise thinshelled brachiopods, ammonites, planktonic foraminifera, sponge spicules and radiolaria. The emphases in this paper are as follows. (1)Sedimentary environments of the siliceous rocks The carbonate rock types with siliceous nodules in the study area include micritic limestones, muddy limestones and wackestones, indicating moderate to low-energy sedimentary environments. It can be seen from Figs. 3 and 4 that sedimentary environments of the nodular or striped siliceous rocks are assembled by open-sea carbonate platform and semi-restricted platform, whereas the thin-bedded siliceous rocks were formed in intraplatformal basin environments. The shallow-sea carbonate sediments were of widespread occurrence in southern Anhui and its adjacent area during the Qixiaian. Till the Gufengian, the southern part of the Susong-Guichi-Tongling-Jingxian-Jingdezhen zone remained to be the shallow-sea carbonate sediments, whilst in the northern part of it, the deeper-water intraplatformal basin sediments predominated as a result of the crustal differential movement, leading to the formation of the intercalations of the thin-bedded siliceous rocks and muddy shales. (2)The genesis of the siliceous rocks The thin-bedded siliceous rocks in the study area are thought to be organogenic deposits which were formed through organic chemical sedimentation and early diagenetic differentiation, whereas the nodular siliceous rocks were resulted from early diagenetic silicification along the bedding plane of the carbonate rocks. (3)The sources of SiO2 SiO2 in the siliceous rocks was principally derived from terrigenous mud and siliceous organisms. By and large, SiO2 in the nodular siliceous rocks was originated from terrigenous mud, i.e. the chemical. weathering products of the continental Al-silicates, whereas SiO2 in the thin-bedded siliceous rocks was mainly stemmed from siliceous organisms which are made up of 30—60% of siliceous sponges and radiolaria. (4)The diagenesis of the siliceous rocks A series of diagenetic processes once took place after the deposition of the abundant siliceous sediments. Three diagenetic stages include: 1)the solution of silica gel or crystalline opal(Opal-A); 2)the reprecipitation(including silicification)and redistribution(i.e. differential deposition)of the disordered cristobalite(Opal-CT), and 3)the formation of micro-crystalline quartz and chalcedony from Opal-CT by solid-solid reaction.