Natural habitats of the Iranian reptiles in many areas of the country are destroying due to several reasons. In such conditions the protected areas can act as the shelter sites for many organisms. Therefore it seems quite necessary that, under management
Masoud Yousefi +4 more
doaj
Analysis of teleseismic P waves with a 5200-station array in Long Beach, California: Evidence for an abrupt boundary to Inner Borderland rifting [PDF]
We analyze teleseismic P waves from four Mw ≥ 6.5 earthquakes recorded by a petroleum industry survey in Long Beach, California. The survey used a 2-D array with up to 5200 seismometers, 120 m mean spacing, and 7 – 10 km aperture.
Clayton, Robert W., Schmandt, Brandon
core +2 more sources
Modelling Neanderthals' dispersal routes from Caucasus towards east. [PDF]
Ghasidian E +4 more
europepmc +1 more source
Geostatistical modeling and spatial distribution analysis of porosity and permeability in the Shurijeh-B reservoir of Khangiran gas field in Iran [PDF]
The main objectives of this study are analysis of spatial behavior of the porosity and permeability, presenting direction of anisotropy for each variable and describing variation of these parameters in Shurijeh B gas reservoir in Khangiran gas field ...
A Hasanipak +16 more
core +1 more source
Phylogeny and Historical Biogeography of Veronica Subgenus Pentasepalae (Plantaginaceae): Evidence for Its Origin and Subsequent Dispersal. [PDF]
Doostmohammadi M +3 more
europepmc +1 more source
Local and regional P-wave spectral attenuation model for Iran. [PDF]
Moradian Bajestani E +2 more
europepmc +1 more source
Stratigraphy 12 (2) Biostratigraphy of the Cambrian-Ordovician boundary beds at Kopet-Dagh, Iran [PDF]
: A continuous succession comprising upper Cambrian (Furongian) to Lower Ordovician (Tremadocian) conodont biozones is reported for the first time from the Kopet-Dagh Region of northeastern Iran.
A P Karpinskii +9 more
core
1-Introduction: Kopeh-Dagh sedimentary basin is located in NE of Iran and is mainly composed of Mesozoic and Cenozoic sedimentary rocks (35 30ˊ-38 15ˊ N, 54 00-61 31ˊE)(Afshar-Harb 1994).
Mohsen Allameh +2 more
doaj
SEISMOGENIC NODES DEFINED BY PATTERN RECOGNITION IN THE CENTRAL PART OF THE ALPINEHIMALAYAN BELT [PDF]
Information on the areas prone to the strongest earthquakes in a region is very important for knowledgeable seismic hazard and risk assessment. We consider the central part of the Alpine-Himalayan Belt (Caucasus–Kopet Dagh-Alburz) for the recognition of ...
Gorshkov, A., Novikova, O.
core +1 more source

