نتایج جستجو برای: Qulqula Radiolarian Formation

تعداد نتایج: 527562  

Journal: :iranian journal of earth science 0
kamal h. karim department of geology, university of sulaimani, kurdistan region, iraq nabaz r.h. aziz department of geology, university of sulaimani, kurdistan region, iraq al-bidary mayssa a.a.a department of geology,university of baghdad, iraq

the asinawa iron ore is located about 3km to the southeast of penjween town, sulaimaniya governorate, kurdistan region, northeastern iraq near the iraq-iran border. the exposed iron ore deposit is about 60 and 400m wide and long respectively. the present study is the re-study of the geology and geochemistry of the asnawan iron ore deposit  and concluded that the country rocks are consist of hor...

Al-Bidary Mayssa A.A.A Kamal H. Karim, Nabaz R.H. Aziz

   The Asinawa iron ore is located about 3km to the southeast of Penjween town, Sulaimaniya Governorate, Kurdistan Region, Northeastern Iraq near the Iraq-Iran border. The exposed iron ore deposit is about 60 and 400m wide and long respectively. The present study is the re-study of the geology and geochemistry of the Asnawan Iron ore deposit  and concluded that the country rocks are consist of ...

Journal: Geopersia 2015

The investigated section cropping out in Kuh-e-Banesh, Zagros basin (southern Iran) is represented by limestone, Cherty beds and marllevels bearing abundant Planktonic foraminifers, radiolarian microfaunas, and ammonite imprints. For the first time, well to moderatelypreserved forms of Planktonic foraminifera have been extracted from black shale and marls levels. Extracted biota was studied wit...

Journal: :geopersia 2015
mazaher yavari mehdi yazdi hormoz gahalavand mohammad hossein adabi

the investigated section cropping out in kuh-e-banesh, zagros basin (southern iran) is represented by limestone, cherty beds and marllevels bearing abundant planktonic foraminifers, radiolarian microfaunas, and ammonite imprints. for the first time, well to moderatelypreserved forms of planktonic foraminifera have been extracted from black shale and marls levels. extracted biota was studied wit...

Journal: :Iraqi geological journal 2022

The radiolarian chert rocks are one of the most important indications existence ophiolites because they a source silica supply. These have been studied to refute and reject idea that do not existed. Si/(Si+Al+Fe+Ca) ratio in indicates is biogenic origin adds SiO2 from shale fraction through diagenetic processes. high values Fe2O3 content indicate hydrothermal effect during precipitation. This c...

Journal: :Berita Sedimentologi 2023

Late Cretaceous (Cenomanian–Turonian) radiolarian fauna was recovered from a single chert sample of the Noni Formation in Miomaffo District West Timor, which is generally viewed as part allochthonous ‘Banda Terrane’. This characterized by presence Cryptamphorella conara, Diacantocapsa euganea, Dictyomitra formosa, montisserei, Guttacapsa biacuta, Stichomitra communis, Patelula verteroensis, Pes...

2015
Jonathan J. Wilson Elizabeth Harding Mathilde Fortier Benjamin James Megan Donnett Alasdair Kerslake Alice O’Leary Ningyu Zhang Kate Jeffery

We tested whether mice can represent locations distributed throughout three-dimensional space, by developing a novel three-dimensional radial arm maze. The three-dimensional radial maze, or "radiolarian" maze, consists of a central spherical core from which arms project in all directions. Mice learn to retrieve food from the ends of the arms without omitting any arms or re-visiting depleted one...

2017
Alexander Matul Rahul Mohan

An objective of the study is to get new biogeographic information on the modern polycystine radiolarians from the high-latitude North Atlantic. The quantitative radiolarian dataset was compiled from publications and own micropaleontological counts from samples of the bottom surface sediments of the North Atlantic north of 40N and Nordic Seas. Standard statistical treatment of micropaleontologic...

2002
THEO ANDREW ALASTAIR H. F ROBERTSON

The Beyşehir–Hoyran–Hadim Nappes crop out over 700 km from NW to SE. Above a regionally autochthonous Tauride carbonate platform the Beyşehir–Hoyran Nappes begin with a thrust sheet (c. 400 m) of mainly redeposited carbonates, quartzose sandstones and mudstones of Mid–Late Triassic age, interpreted as a proximal slope–base-of-slope succession. Above is a thrust sheet (c. 1 km) of Middle–Upper T...

نمودار تعداد نتایج جستجو در هر سال

با کلیک روی نمودار نتایج را به سال انتشار فیلتر کنید