The shoal(or bank) and shoal facies are important types of carbonate deposits. The bioclastic shoal and ooid shoal are common in geological history. In general, the shoal (or bank) includes bar, ridge, mound and other sedimentary bodies. The envirnoment and state of shoal should be considered while the shoal is analyzed. Many examples of ancient and modern ooid shoals show its complex natures. For example, the ooid shoal not only developed on platform, margin, but also developed in coast zone, and the ooid deposit not only occurred in bar, but also occurred in tidal delta, ridge, sheet, tidal flat, lagoon, etc..;
出版日期: 1999-06-01
作者简介: 沙庆安,男,1933年生,现为中国科学院地质研究所研究员,长期从事沉积学研究工作。
引用本文:
. 关于滩相沉积[J]. 古地理学报, 1999, 1(3): 8-12.
. STUDY ON SHOAL FACIES DEPOSIT[J]. JOPC, 1999, 1(3): 8-12.
1辞海编辑委员会.辞海.上海辞书出版社,1979.2254
2汉语大词典编辑委员会,汉语大词典编篡处.汉语大词典.上海:上海辞书出版社,1986.219
3英汉地质词典编辑组.英汉地质词典.北京:地质出版社,1983.804,972
4Bates R L, Jaclson J A. Glossary of Geology(3rd ed). America Geological Institute: Alexandria Virginia, 1987.53,54,609
5Loean J P, Purser B H. Distribution and ultrastructure of Holocene ooids in the Persian Gulf. In:Purser B H, eds. The Persian Gulf, Holocene carbonate sedimentation and diagenesis in a shallow epicontinental sea. Springer Verlay,1973.279~328
6Halley R B, Harris P M, Hine A C. Bank marginal environment. In:Scholle P A, Bebout D G, Moore C H, eds. Carbonate depositional environmets.AAPG memoir, 1983,33:463~506
7Zeng Yunfu, Nan Hao Lee, Yang Zhoun Huang. Sedimentary characteristics of oolite carbonate from the Jialing Jiang Formation (Lower TriassicTJ), South Sichuan Basin, China. In: Seryt T M, ed. Coated grains II. Springer verlag,1983,10:176~1878沙庆安,江茂生.鲕滩相与藻坪相沉积
[CD2]鲁西地区中寒武统张夏组剖析.沉积学报,1998,16(4):62~71