Results 181 to 190 of about 1,902 (206)
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Geology and Petroleum Potential of the Makran Coast, Pakistan
Proceedings of Offshore South East Asia Show, 1982Coastal Makran is generally acknowledged as a subduction zone where the Indian Ocean plate moves northward under continental crust. The geologic history deduced from facies and structures is complex and can be divided into three major episodes :A Middle Miocene and older phase dominated by turbidity currentdeposition on a vast deep-sea fan which ...
J.C. Harms, D.C. Francis
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Microplastics in the surface seawaters of Chabahar Bay, Gulf of Oman (Makran Coasts)
Marine Pollution Bulletin, 2019Current study aimed to evaluate the microplastics abundance in the surface waters of Chabahar Bay for the first time. 21 neuston net water samples were collected from 7 stations. Microplastics were visually counted by stereomicroscope, sorted into 4 size categories, 4 shape categories, and identified by ATR-FTIR spectroscopy.
Mojgan Khamarzadeh, Aliabad +2 more
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Harappan Outposts on the Makran Coast
Antiquity, 1962The widespread remains of the Indus Valley or Harappan civilization—contemporaneous in part with the great civilizations of Mesopotamia and Egypt—present at first glance a picture of sterile isolationism. Yet none of the great civilizations of the world originated or thrived in a cultural and economic vacuum.
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UPLIFTED MARINE TERRACES ALONG THE MAKRAN COAST OF PAKISTAN AND IRAN
2002The Makran coast of Pakistan and Iran is dominated by spectacular marine terraces of greater size and extent than most other coasts of the world. This terraced coast extends >1000 km from near Karachi, Pakistan, to Jask, Iran, near the entrance to the Strait of Hormuz.
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Morphometric characteristics of three species of Gobiidae family in Makran coast
2021Tabatabaei Yazdi, Fatemeh +2 more
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On the generation and propagation of Makran swells in the Arabian Sea
International Journal of Climatology, 2020Anoop Tr +2 more
exaly
Investigating an upwelling system along the eastern Makran coast
Zoljoodi Zarandi M., et al.openaire +1 more source

