Results 101 to 110 of about 884,714 (212)

Aquathermolytic Upgrading of Zarafshanian Extra Heavy Oil Using Ammonium Alum. [PDF]

Molecules
Ali Akhunov A, Aliev F, Mukhamadiev N, Kahwir OF, Dengaev A, Majeed MY, Esmaeel M, Al-Qaz A, Mirzaev O, Vakhin A.   +9 more
europepmc   +1 more source

Deciphering the collisional dynamics of the Bangong-Nujiang Tethyan Ocean: multi-regional anisotropy of magnetic susceptibility (AMS) constraints from the Central Tibetan Plateau. [PDF]

Sci Rep
Chen Q, Cheng X, Jiang N, Wei B, Xing L, Zhang D, Chai R, Wu H.   +7 more
europepmc   +1 more source

An archaeal virus capable of hydrolyzing the surface glycan of the host cell. [PDF]

mLife
Yuan W, Pei C, Huang J, Chen H, Fan J, Jin C, Huang L.   +6 more
europepmc   +1 more source

THE QUENAST PLUG: A MEGA-PORPHYROCLAST DURING THE BRABANTIAN OROGENY (SENNE VALLEY, BRABANT MASSIF) [PDF]

, 2008
Debacker, Timothy, SINTUBIN, M
core   +1 more source

Gold geochemical anomalies delineated by the stratigraphic zoning anomaly lower limit contrast method: a case study of panjiaba, Shaanxi province, China. [PDF]

Sci Rep
Yuekun W, Shaolei K, Jin L, Shangqi L, Chaoran D.   +4 more
europepmc   +1 more source

Hydrogen Embrittlement Behavior and Applicability of X52 Steel in Pure Hydrogen Pipelines. [PDF]

Materials (Basel)
Li T, Zhang H, Hu W, Li K, Wang Y, Lin Y.   +5 more
europepmc   +1 more source

Geological evolution of the Pietersburg greenstonebelt, South Africa and associated gold mineralization [PDF]

The polyphase history of gold mineralization seen in the Pietersburg greenstone belt is integrated with the geochemical and tectonic evolution of greenstone belts as a whole.
Dewit, M. J., Jones, M. G.
core   +1 more source

Characterization of talc deposits in ultramafic rocks of Gebel El Maiyit and its economic feasibility. [PDF]

Sci Rep
Salem IA, Aly SM, Shebl A, Thabet IA.
europepmc   +1 more source

Lithology, age and structure of early proterozoic greenstone belts, West African shield [PDF]

Lithologic and chemical data have been compiled for belts in the Proterozoic terrane. Available stratigraphic information from geologic maps of these areas indicate that a typical sequence is comprised of predominately mafic lava flows (basalt-andesite ...
Attoh, K.
core   +1 more source

Metasomatism of the carbonate rocks of the contact zone with the basalt. [PDF]

Sci Rep
Stanienda-Pilecki KJ.
europepmc   +1 more source