marine transgression
2.Study on coal accumulation under marine transgression events in the epicontinental basin of North China
3.THE FUSULIND ACME-ZONE AND THE CANON OF LATE CARBONOFEROUS MARINE TRANSGRESSION IN NORTH CHINA
4.HOLOCENE MARINE TRANSGRESSION AND ITS MICROP ALEONTOLOGICAL CHARACTERISTICS IN THE NORTH-EASTERN WATERS OF BEIBU GULF
5.Pinghu formation of Eocene in Xihu sag of the shelf basin of the East China Sea is semi-closed bay sedimentary environment. Marine transgression is from south to north.
6.While from west to northeast the average values of 87 Sr / 86 Sr are increasing in plane,indi cating that the marine transgression during the Carboniferous period happened in direction from west toward east.
7.Based on the analyses of grain size, clay minerals, carbonate and dating of paleomagnetism for the core of 450m from Wuhaozhuang, it has been revealed that the Huanghe Delta has undergone secular and stable deposition since the late Pliocene (380×10~4a) and deposited mainly the sediments of river-lake facies consisting of silty mud, muddy silt and fine-sand and a little sediments of marine facies locally affected by the transgression of the Bohai Sea during the late Pleistocene.
8.The scholars insisting on transgression provided many markers such as mineralogy, lithology, paleoecology and geochemistry, but these makers are not completely the same as normal marine makers, moreover, the passageway and obviously increased makers of transgression have not been discovered, so "marine flooding", "tsunami" and "terrestrial facies" appear, these viewpoints have coexisted for a long time.
9.Sequence correlation shows Silurian transgression onlapped from northwest to southeast direction. The sandstonebody, developed in transgression system tract (TST), better reservoir are mainly located near the maximum marine flooding surface, i.e. thefavorable position for marine sandstone body development would be the upper part of TST and the lower part of high system tract (HST).
