波—流相互作用机制与复合流的沉积构造鉴别标志*
Mechanism of wave-current interaction and identification of sedimentary structures of combined-flow
Li Xiang-Dong
波—流相互作用机制与复合流的沉积构造鉴别标志* |
|
李向东 |
Mechanism of wave-current interaction and identification of sedimentary structures of combined-flow |
|
Li Xiang-Dong
|
| 典型的复合流沉积构造 a—复合流波痕( Basilici et al ., 2012 );b—复合流层理( 李向东等,2010 );c—爬升型复合流层理( Lamb et al ., 2008 );d—不对称丘状交错层理( McKie,1994 );e—准平行层理( Arnott,1993 );f—近水平或不规则侵蚀面(红线)和频繁交替出现的浪成波纹层理和流水层理,且两者发育均不充分,其中T为潮汐成因构造,W为波浪成因构造,f1至f7为沉积构造自下而上可分为7组( Meene et al ., 1996 ) |
| |