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Chung, Y. United States. Cooperative Inst. It has been discussed that the greenhouse gases, e. Many scientists are therefore interested in monitoring the minor constituents of the atmosphere and in the carbon cycle. Here the four year monitoring of the trace gases at the three sites in East Asia is reported. The results are also compared with the measured values obtained at the free troposphere background site at MLO in Hawaii.
Petrology of Ortsog- Uul peridotite-gabbro massif in Western Mongolia. The Ortsog- Uul mafic-ultramafic massif of Western Mongolia is located in a tectonic block with overturned bedding. The massif hosts two intrusions: a rhythmically-layered peridotite-gabbro association Intrusion 1 and massive Bt-bearing amphibole-olivine gabbro Intrusion 2. Intrusions 1 and 2 have different petrology features.
The chondrite-normalized REE and primitive mantle-normalized rare elements patterns of Ortsog- Uul intrusions have similar curves of elements distribution.
However, Intrusion 2 is characterized higher contents of REE and rare elements. High concentrations of incompatible elements are indicative of strong fractionation process. It has been suggested that Intrusions 1 and 2 derived from compositionally different parental melts. The concentration of MgO in melt is The circular Uneged Uul structure East Gobi Basin, Mongolia - Geomorphic and structural evidence for meteorite impact into an unconsolidated coarse-clastic target?
As revealed by remote sensing and recent field reconnaissance, the central part of the Uneged Uul structure comprises a complex central peak of outward-radiating curved ridges, composed of stratigraphically uplifted greenschist-facies basement schists, surrounded by an annular moat. Jurassic conglomerates forming the main part of the central annular ridge show effects of severe internal deformation.