The formation of slope streaks is among the few active processes know to be occurring on the red planet.
This technique has been used for varied characteristics of drainage basin, which include erosion surfaces, nature of erosion and formation of slope.
The formation of initial slope clinoforms is closely related to movement along the underlying basement fault in the eastern Qiongdongnan area.
Reactivation of pre-existing strike-slip faults in the Yinggehai area and extensional faults in the Qiongdongnan area resulted in the formation of initial slope clinoforms during the Miocene post-rifting stage.
The formation of the bend slope break belt caused the steep slope fault belt to become an up-dip foot slope belt (Fig. 6).
The geological structure and calcareous nannofossil biostratigraphy of the Middle to Late Miocene trench-slope succession in the southern Boso Peninsula, central Japan, were examined to obtain chronological constraints on the accretion and formation of the trench-slope architecture.
Researchers have found that long-term active syndepositional faults are the predominant controlling factor in formation of various structural slope break belts in continental rift basins (Lin et al. 2000; Wang et al. 2004; Ren et al. 2004; Feng 2006).
The processing improvement, a synthesizing technique based on the SMQ process, was established which allowed the segregation control and inhibited second-phase transformation, thus avoiding formation of a plateau-slope.
The formation of the reef slope also indicates low current as there are vertical 'sediment rain' grooves and a lack of filter-feeding organisms below 150 m but the presence of suspension feeding crinoids and echiurid worms.
Several abiotic factors impact the formation of microrefugia including slope, exposure, and elevation [ 10].
The other kind of reservoir developed in the middle Miocene Meishan Formation, which compose of slope break-controlled submarine fan.
