scholarly journals Regional stream sediment and water geochemical data, Nahoni Range area, west-central Yukon (parts of NTS 116F, G and K)

2008 ◽  
Author(s):  
P W B Friske ◽  
M W McCurdy ◽  
S J A Day ◽  
R J McNeil ◽  
A G Grenier
Keyword(s):  
Stream Sediment ◽  
Geochemical Data ◽  
West Central

Multivariate Analysis of Stream Sediment Geochemical Data for Gold Exploration in Delijan, Iran

2018 ◽  
Vol 5 (2) ◽  
pp. 325-334
Author(s):  
Farid Javadnejad ◽  
◽  
Javad EskandariShahraki ◽  
Sanaz Khoubani ◽  
Elham Kalantari ◽  
...  
Keyword(s):  
Multivariate Analysis ◽  
Stream Sediment ◽  
Geochemical Data ◽  
Gold Exploration

scholarly journals Granulometry, heavy mineral and geochemical studies of stream sediments around Bula, Dass District, Northeast Nigeria

2020 ◽  
Vol 18 ◽  
pp. 63-73
Author(s):  
C. I. Adamu ◽  
E.E. Okon ◽  
D.O. Inyang
Keyword(s):  
Trace Elements ◽  
Stream Sediments ◽  
Stream Sediment ◽  
Heavy Mineral ◽  
Geochemical Data ◽  
Provenance Analysis ◽  
Sediment Samples ◽  
Granulometric Analysis ◽  
Elemental Analyses ◽  
Geochemical Studies

Active stream sediments generally consist of broken-down fragments of pre-existing rocks by the action of river (stream) flow. This makes them target materials for routine geochemical surveys and provenance analysis. Fifteen (15) stream sediment samples were collected in some parts of Bula and its environs, northeastern Nigeria, in order to determine their textural characteristics, heavy mineral and elemental composition. The sediments were subjected to granulometric, heavy mineral and elemental analyses. The result of granulometric analysis show that the streamsediments are poorly to moderately well sorted, very platykurtic to leptokurtic, fine to medium grained and positively skewed. Zircon, rutile and tourmaline are the dominant heavy mineral species occurring in the sediments. The computed Zircon-Tourmaline-Rutile (ZTR) index values for the samples range from 59.18 - 83.53, indicating mineralogical maturity. The geochemical data of the stream sediment samples show that the mean contents of the trace elements [Ti (0.73 ± 0.74%), Fe (0.39±0.19%), Cr (816±639ppm), Ni (258±108ppm), Pb (48±12.37ppm) and Zn (502±126ppm)] were higher than their respective average crustal values except for Fe. Computed threshold values indicate possible mineralization containing Fe and Ti. The elements have variable spatial distribution. The study shows that the trace elements composition of the stream sediments is majorly lithogenic. Because mineralization in rocks and sediments are often characterized by considerable variation in their trace elements contents, the metal concentrations in these sediments are large enough for Ilmenite and Rutile mineralization to be suspected within the study area.

scholarly journals Regional stream sediment and water geochemical data, Lansing Range area, east central Yukon (NTS 105N)

2009 ◽  
Author(s):  
S J A Day ◽  
M W McCurdy ◽  
P W B Friske ◽  
R J McNeil ◽  
E H W Hornbrook ◽  
...  
Keyword(s):  
Stream Sediment ◽  
Geochemical Data ◽  
East Central
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