SPATIAL DISTRIBUTION ANALYSIS OF LOESS DEPOSITS IN SOUTH AND SOUTHEAST OF CASPIAN SEA

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GHANAVATI EZATOLLAH; MOHAMMADI ZAKIEH

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Journal: Physical Geography Research Year:2014 | Volume:45 | Issue:4 Page(s): 7-9

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Title

SPATIAL DISTRIBUTION ANALYSIS OF LOESS DEPOSITS IN SOUTH AND SOUTHEAST OF CASPIAN SEA

Author(s)

GHANAVATI EZATOLLAH | MOHAMMADI ZAKIEH | Issue Writer Certificate

Keywords

GEOMORPHOLOGYQ1

LOESSQ2

SOUTH AND SOUTH EAST OF CASPIAN SEAQ2

SPATIAL ANALYSISQ2

Abstract

Introduction The word “Loess” has been derived from the German word “Los”, meaning LOESS, which was used for the first time by Leonard in 1824. Regarding the definition of LOESS presented by many authors, aeolian origin and silt fraction dominance have been accepted as the two main attributes of LOESS deposits. Wind- blown deposits of LOESS are characterized by a lack of stratification and uniform sorting and occur as blanket deposits (Bell, 2000). The common mineralogical composition of LOESS deposits is as follows: quartz, feldspars, carbonates, mica and heavy minerals in the silt fraction. According to Pye (1995), four fundamental requirements are necessary for its formation; a dust source, adequate wind energy to transport the dust, a suitable accumulation area, and a sufficient amount of time.

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APA: Copy

GHANAVATI, EZATOLLAH, & MOHAMMADI, ZAKIEH. (2014). SPATIAL DISTRIBUTION ANALYSIS OF LOESS DEPOSITS IN SOUTH AND SOUTHEAST OF CASPIAN SEA. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, 45(4), 7-9. SID. https://sid.ir/paper/405947/en

Vancouver: Copy

GHANAVATI EZATOLLAH, MOHAMMADI ZAKIEH. SPATIAL DISTRIBUTION ANALYSIS OF LOESS DEPOSITS IN SOUTH AND SOUTHEAST OF CASPIAN SEA. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY[Internet]. 2014;45(4):7-9. Available from: https://sid.ir/paper/405947/en

IEEE: Copy

EZATOLLAH GHANAVATI, and ZAKIEH MOHAMMADI, “SPATIAL DISTRIBUTION ANALYSIS OF LOESS DEPOSITS IN SOUTH AND SOUTHEAST OF CASPIAN SEA,” PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, vol. 45, no. 4, pp. 7–9, 2014, [Online]. Available: https://sid.ir/paper/405947/en

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