Sentence examples for early highstand systems from inspiring English sources

The lower subunit represents hemipelagic and prodeltaic deposition of the transgressive and early highstand systems tracts.

When the rate of sea level rise decreased strongly, the shoreline migrated seaward and prograding and aggrading sandy material, with landward muddy lateral equivalent facies, deposited early highstand systems tract (HST) above the MFS.

The early highstand system tract during the Early Maastrichtian notably shows a decrease in the planktonic/benthoic ratio and is combined with increasing carbonate beds, as well as decreasing marl beds, from both the thickness and frequency points of view, and this points to a slow rate of sea level rise while the depositional rate exceeds it (Table 3).

The early seismic sequence divides into a lowstand systems tract (LST), transgressive systems tract (TST) and highstand systems tract (HST).

Major palaeoenvironmental changes include the rapid landward migration of a barrier-estuary lagoon system during the Early–Middle Holocene (transgressive systems tract—TST), followed barrier-estuary lagoongradation in the lasystem0 yr (highstanduringems thect—HST).

A highstand systems tract (HST) is recognized in the Eocene Shahejie Formation in eastern Dongying depression.

Each sequence consists of two systems tracts: a transgressive systems tract and a highstand systems tract.

A sea/lake level rise can either form a highstand systems tract (HST) or a transgressive and an overlying highstand systems tract (HST), depending on the sediment supply.

Later on, as lake level continuously rose, transgressive and highstand systems tracts were developed.

The Holocene seismic sequence comprises a type 1 sequence with lowstand, transgressive and highstand systems tracts.

Transgressive and highstand systems tracts were resolved based on such facies stacking patterns.