Since 1960's

the study of deep-water tractive current deposits has become a new research field in sedimentology. The present studies on deep-water tiactive current deposits are mainly focused on contourits current deposit

internal-tide and internal-wave deposits. Considerable progress has been made in the study of contourite corrent depositssince mid-1960's

especially in the study of modern contourite deposits. Now deep understanding has made on the formation mechenism

the characteristics of texture and structure

the vertical sequences

the rock facies and recognition marks of contourite deposits. The discovery of contourite-dome is the most important and distinctve achievement in this field. Numerous large-scale modern contourite-dome

which can be compared with deep-water turbidite fans

were discovered in deep-water oceanic areas and in stratigraphic record. The study on internal-tide and internal-wave deposits began in the early 1990's and developed rapidly

and has made considerable progress in the formation mechanism

the characteristics of texture and structure

the vertical sequences

the rock facies and arcognition marks. The Ordovician internal-tide and internal-wave deposits in West Zhejiang and Tarim Basin are typical cases in this field. Compared withturibidities

the deep-water tractive current deposits are more favourible in the reservoir characteristics

and have veryimportant oil-gas-bearing potential.