Contrasting Evolutionary Trajectories: Differential Population Dynamics and Gene Flow Patterns in Sympatric <i>Halimeda discoidea</i> and <i>Halimeda macroloba</i>. [PDF]
Tong Y, Liu W, Sun Y, Liu J, Yang Q.
europepmc +1 more source
Groundwater resources: challenges and future opportunities. [PDF]
Mukherjee A +3 more
europepmc +1 more source
Anomalous dynamic response and micro-zonation of saline sabkha soils of eastern Saudi Arabia using 3D seismic behavior modelling. [PDF]
Fayyaz M +4 more
europepmc +1 more source
<sup>222</sup>Rn, <sup>226</sup>Ra, and <sup>238</sup>U in soil samples at a depth of 50 cm in KUFA City of AL-NAJAF Governorate, IRAQ. [PDF]
Rashed EM, Abojassim AA, Jassim AS.
europepmc +1 more source
Cyclic CO<sub>2</sub> Injection Process Recovery Behavior in Classified Deep Formations. [PDF]
Li Y, He J, Hu C, Wang W, Wan T.
europepmc +1 more source
Related searches:
Geology of the Ozark Lead Company Mine, Viburnum Trend, Southeast Missouri
Economic Geology, 1977In contrast to most of the other mines in the Viburnum Trend, much of the Ozark Lead Company orebody lies at right angles to the depositional strike of the sediments. This divergence is due to localization of much of the ore along the flank of a northwest-trending Precambrian high situated on the upthrown side of a high-angle reverse fault.A second ...
M. M. Mouat, C. W. Clendenin
openaire +1 more source
The geology of the Aguilar lead-zinc mine, Argentina
Economic Geology, 1950"The Aguilar deposit, in northern Argentina, is a hypothermal lead, zinc, silver replacement in Cambrian calcareous quartzite. The rocks had previously been altered to tactite by a granite stock whose contact is from 150 to 250 m. from the ore bodies.
openaire +1 more source
The geology of the Zawar lead-zinc mine; a reply
Economic Geology, 1968Reply is made to several critical discussions published since the publication of the original paper in 1964 (for reference, see this Bibliography Vol. 29, Mookherjee 1; see also Vol. 29, Mookherjee 2; Vol. 30, Poddar 2; Vol. 31, No. 4, 02 E67-02447; Vol. 32, No. 1, 02 E68-00608). The deposit is regarded as a product of ascending hydrothermal solutions.
openaire +1 more source

