QUATERNARY JOURNAL OF IRAN
Year:2016 | Volume:2 | Issue:2|Papers Count:7

1-Introduction: Environmental changes, such as changes in lake levels and changes alluvial environment and its effects on the settlement pattern of archaeological sites, represent the human dependence on environmental resources. Findings of the Zagros region, suggesting climate change and the environment and creating opportunities and threats to human societies in the past. Archaeological evidence shows that human societies during the Holocene in settlements located in this area have been established.

Cham-e Souran, Paleolithic, Source routing, Zagros Cham-e souran is located on Ravand basin on the west side of Larini Adjudan village, which is on the east side of Islam Abad, Kermanshah. It includes the wide area and an open site of Paleolithic that is formed on an exposed ophiolite.

This study provides morphology and field survey data on Ghasr-e-Ghand and Kahorkan thrusts, in the central part of eastern Makran accretionary wedge, in southeast Iran.

Behashtabad Damsite is located in High Zagros Zone, at 6-km distance from the south of Ardal Thrust Fault and 7-km from the north of Dopolan Thrust Fault. The outcropped deposits in the studied area locate in Zagros thrust zone. Paleozoic deposits contain red shales and sands belonging to Cambrian. Mesozoic deposits mostly belong to Cretaceous.

1-Introduction: The Institute of geophysics of Tehran University is establishing a luminescence sample preparation laboratory. The following investigations and experiments was performed to find the safe light for this lab. This paper is written in Farsi to provide answer to many questions that the first author has been asked locally about which light is suitable for both sample preparation lab and in the field during sampling in dark.

1-Intrudaction: One of the evidences of the Quaternary climate changes in Iran, are glacial topography in mountainous areas. Understanding glacier forms such as cirques, as the accumulation of snow and ice sites and mountain glaciers supply, is very important in glacial geomorphology.

1-Introduction: Examinations of sedimentological and mineralogical characteristics of the closed-basin cores due to the very high susceptibility to precipitation and evaporation balance are beneficial for determination and evolution of late Quaternary sedimentary specification.