Zobrazeno 1 - 10
of 2 396
pro vyhledávání: '"S. A. de Waal"'
Autor:
S. A. de Waal
Publikováno v:
South African Journal of Geology. 115:345-368
Burnt Mountain is the name attached to a series of low, dark-coloured hills, dominantly composed of carbonaceous shale, siltstone, sandstone and various ferruginous rocks belonging to the Permian Verbrande Berg Formation, Ecca Group, Karoo Supergroup
Autor:
Lu, Ping1 (AUTHOR), Yang, Shihan2 (AUTHOR), Shi, Yushuang1 (AUTHOR), Wang, Na1 (AUTHOR), Ding, Beijing1 (AUTHOR), Liu, Weijie1 (AUTHOR), Zhang, Pei1 (AUTHOR) pdgujunjun@163.com, Rong, Lan3 (AUTHOR) rl20816@rjh.com.cn, Bian, Dongsheng2 (AUTHOR) biandd1211@163.com
Publikováno v:
BMC Nursing. 12/4/2024, Vol. 23 Issue 1, p1-9. 9p.
Autor:
Yıldırım, Tuğba Öztürk1 (AUTHOR) tugba.ozturkyildirim@gmail.com, Karatepe, Hilal Kuşcu2 (AUTHOR)
Publikováno v:
BMC Nursing. 11/11/2024, Vol. 23 Issue 1, p1-10. 10p.
Publikováno v:
Journal of African Earth Sciences. 50:111-119
The combination of ion microprobe dating and cathodoluminescence (CL) imaging of zircons from a high-grade rock from the Central Zone of the Limpopo Belt were used to constrain the age of metamorphic events in the area. Zircon grains extracted from a
Publikováno v:
South African Journal of Geology. 109:279-300
The Lindeques Drift and Heidelberg Intrusions and the volcanic Roodekraal Complex belong to a high-Ti mafic igneous suite (HITIS) that was emplaced in the Kaapvaal Craton as km-sized bodies, to the north and north-east of the Vredefort impact structu
Publikováno v:
Journal of African Earth Sciences. 43:537-548
The Schurwedraai alkali granite is one of a number of prominent ultramafic-mafic and felsic intrusions in the Neoarchaean to Palaeoproterozoic sub-vertical supracrustal collar rocks of the Vredefort Dome, South Africa. The alkali granite intruded the
Publikováno v:
Mineralogical Magazine. 67:1015-1021
We report in this paper the first occurrence of the rare assemblage corundum + quartz in the high-grade metamorphic zone in the core of the Namaqualand Metamorphic Complex (NMC) (South Africa). The magnetite-bearing rocks hosting the corundum-quartz
Autor:
McCarthy, T. S., Schweitzer, J. K., Seymore, W., Ogilvie, P., de Waal, S. A., Govender, A., Weise, S., Pretorius, H., Wagner, L., Naicker, B.
Publikováno v:
South African Journal of Geology; Jun2024, Vol. 127 Issue 2, p285-324, 40p
Publikováno v:
South African Journal of Geology. 104:343-354
Mafic-ultramafic sills of up to 450m in thickness occur near the contact between sedimentary and volcanic rocks of the Silverton Formation, Transvaal Supergroup, on the farms Blaauwboschkraal, Zwartkopje and Waterval, some 10km north of Waterval Bove
Publikováno v:
South African Journal of Geology. 104:309-318
Both Ni-Cu and PGE deposits are associated with mafic and ultramafic rocks, but the former often occur in dynamic magmatic systems such as lava channels and magma conduits whereas the later occur in larger layered intrusions. The contrasting modes of