fan delta

Heterogeneity parameters indicate that the heterogeneity of subaqueous distributary channel of (fan) delta-front is the most serious.

Alluvial fan and fan delta distribute on the western slope of the depression, and turbidite fan distributes in lake-basin center.

Various types of fan delta systems have been developed in different evolution stages of faulted basin.

Central low uplifting provides clastic matter for eastern steep slope belt which mainly develops fan delta and nearshore subaqueous fan.

the Upper Cretaceous was in the higher base level, which developed fan delta- lacustrine facies until late Oligocene.

from northern and western to southern and eastern , the sedimentary facies transited from fan delta , braided delta to lake facies.

The research showed the sedimentary facies types include lacustrine, fan-delta facies and braided river delta facies.

They formed in continental faulting basins and their sedimentary facies mainly include river, delta and fan delta.

Lakeshore and fan delta plain of the third stage are the main environments of coal accumulating .

The type of conglomerate is regarded as an important symbol for distinguishing fan delta from braided delta.

The sedimentary facies includes alluvial fan, fan-delta, offshore lake, shallow lake and deep lake facies.

Huludao uplifting provides clastic matter for its periphery area which mainly develops fan delta.

The subaqueous distributary channel is the main type of the fan delta front while the channel mouth bar is developed locally.

Longitudinal delta is developed in the north, fan-delta in the east, and slope progradation complex in the west.

The sedimentary pattern and forming conditions of lithologic traps in the fan delta are analyzed.

There was river way sediment of fan delta in HanDan region according to regional deposition backgrounds and 10 field lithology contrasts.

they are alluvial fan-river (alluvial flat)-delta-lake-lake floor fan model and alluvial fan-fan delta-lake-lake floor fan model.

Fan delta sediments developed well in the northern area of Turpan Depression.

In the lower part of Member 3 of Shahejie Formation, the main reservoir types are fan-delta and sublacustrine fan facies.

Three subfacies are included in the fan delta: fan delta-plain, fan delta-front and fan pro delta.

The gentle slope type slope break belt controlled the development of the fan delta system.

The question is : how many fan-delta does Yellow Car really need to get to London?

It can be divided into 2 subfacies of fan delta-front and fan pro delta, and 6 microfacies.

experimental study of sandy - fan - delta sedimentary process

Sequence evolution of fan-delta outcrops and its controlling on the sandstone reservoirs

Application of stochastic simulation of reservoir parameters on heterogeneity in fan delta reservoir

Recognition and Correlation of Two Distinct Types of Fan Delta Facies

Fan-delta deposits of the pliocene atushi formation in the Southwest Depression, Tarim basin

Development and application of geological knowledge database for fan-delta front in the dense spacing area

High-Resolution Sequence Research in Fan-delta Sedimentary System

The Triassic fan delta facies and the alluvial fan facies are favorable reservoir blocks in this region;

Early Jurassic Alluvial Fan- Fan Delta Depositional System of Delingha Basin and Its Markov Model

The Consideration on the Quantitative Division of Fan Delta Subfacies

Geologic Model for Lithologic Reservoir in Highstand Fan Delta

A Review of Fan Delta Studies at Home and Abroad