Log of diamond drill core, Hole Number 1, Lahuf mine, Saudi Arabia

1967 ◽  
Author(s):  
P.K. Theobald ◽  
Charles Emmet Thompson ◽  
Louis Gonzalez
Keyword(s):  
Saudi Arabia ◽  
Drill Core ◽  
Core Hole ◽  
Diamond Drill ◽  
Hole Number

Geochemical data of diamond drill core samples adjacent to the Red Lake Indian Reservation, northern Minnesota

1993 ◽  
Author(s):  
Warren C. Day ◽  
R.L. Earhart ◽  
Paul H. Briggs ◽  
J.S. Mee ◽  
D.F. Siems ◽  
...  
Keyword(s):  
Geochemical Data ◽  
Drill Core ◽  
Indian Reservation ◽  
Diamond Drill ◽  
Core Samples ◽  
Red Lake

Late Ordovician–earliest Silurian chitinozoans from the Qusaiba-1 core hole (North Central Saudi Arabia) and their relation to the Hirnantian glaciation

2015 ◽  
Vol 212 ◽  
pp. 60-84 ◽  
Author(s):  
Florentin Paris ◽  
Jacques Verniers ◽  
Merrell A. Miller ◽  
Sa'id Al-Hajri ◽  
John Melvin ◽  
...  
Keyword(s):  
Saudi Arabia ◽  
Late Ordovician ◽  
Core Hole ◽  
North Central

Progress report on analyses of pyritic core from diamond drill holes under gossan at Wadi Wassat, Saudi Arabia

1967 ◽  
Author(s):  
William C. Overstreet ◽  
Louis Gonzales ◽  
C.E. Thompson ◽  
Mohammed A. Fourati ◽  
Ali Sharah ◽  
...  
Keyword(s):  
Saudi Arabia ◽  
Progress Report ◽  
Diamond Drill ◽  
Drill Holes

The Goulding–Keene nepheline pegmatite near Bancroft, Ontario

1976 ◽  
Vol 13 (2) ◽  
pp. 237-248 ◽  
Author(s):  
E. J. Reeve ◽  
G. M. Anderson
Keyword(s):  
Original Composition ◽  
Drill Core ◽  
Diamond Drill ◽  
Mineral Analyses

The Goulding–Keene pegmatite consists essentially of albite, nepheline, and biotite with minor amounts of microline and other minerals. It is enclosed by plagioclase–nepheline–biotite–hastingsite–calcite gneisses and is apparently intrusive into these gneisses since it cuts the foliation of the gneisses, has some sharp contacts, and is not itself foliated. The gneisses and the pegmatite were sampled by more than 240 m of diamond drill core. Rock and mineral analyses show that the present composition of the pegmatite is very unlikely to be an igneous composition, and therefore that metasomatism has changed the original composition after emplacement of the pegmatite as a melt. This is consistent with textures observed in the gneisses and pegmatite.

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