late pleistocene

It has ever controlled the earthquakes of ancient and contemporary times and is determined to be probably active since late pleistocene.

To sum up, the earth's crust of the area has a weak activity to show mainly creep-slip active mode since the Late Pleistocene.

Since the Late Pleistocene, the tectonic regime has changed to strike slip and reverse faulting one.

Many geological evidences show however that larger lake and high lake levels once existed in this area during the Late Pleistocene.

The different sedimentary environment at late Pleistocene was mainly due to vertical motion of fault block.

Since the late Pleistocene, the two faults haven' been active.

Bactrian camels, which are critically endangered in the Gobi Desert, could provide a modern proxy for Camelops, a late Pleistocene camel.

In the late Pleistocene, modern water system was formed as the climate was much more drought.

These structures are believed resulting from earthquake related to volcanic activity of the Late Pleistocene.

For instead, this project started to extract ancient DNA from Late Pleistocene mammoth- coelodonta fauna from Northeastern China since 2003.

This led the research team to conclude an extraterrestrial impact wiped out many of the inhabitants of the Late Pleistocene.

Since late Pleistocene, this segment was relatively inactive on the whole.

A recent study has provided clues to predator-prey dynamics in the late Pleistocene era.

This lake lasted about two millions years and vanished in the Late Pleistocene.

During the Late Pleistocene, these caves were dry.

The highest terrace was formed in the Late Pleistocene.

High-resolution paleoceanographic study of the Okinawa Trough Since the late Pleistocene

We believe that the Shenzhen fracture zone had no perceptible activities since late Pleistocene by fault profiles and fault material;

The micro-structural characteristics of the Late Pleistocene loess and its environmental meaning in Xianyang City

Late Pleistocene Sedimentary Stratigraphic Structure and Its Implication in the Central and Western Areas of Southern Yellow Sea

Spore-pollen records of environmental change on south coast plain of Laizhou Bay since the Late Pleistocene

Tectonic Deformation of China Continent and Its Adjacent Regions since Late Pleistocene Inferred from Active Fault Movement Data

Sedimentary Characteristics of Weihe Palaeochannel Since Late Pleistocene and Their Control to Modern Salt-Water Intrusion

Late Pleistocene Marine Dinoflagellate from Dongying Depression, Shandong Province

Valuable heavy minerals and their resource potential on outer shelf in East China Sea during the Late Pleistocene

Vegetation and climate environment during the late Pleistocene in Loess Plateau, China

Volcanic Sediments in the Eastern South China Sea During the Late Pleistocene Epoch

Vegetation and Climate During the Late Pleistocene in Fu County, Shaanxi

U-Series Component Dating for Late Pleistocene Basalt of Longgang, Jilin Province

Human Activities and Lake Evolution in North Qinghai since Late Pleistocene

The Huanghe River course and delta from end of Late Pleistocene to the 7th century BC

Climate variability in the Botswana Kalahari from the late Pleistocene to the present day