By Joan Terry
Towards structural lineaments and predictive hydrothermal porphyry deposits mapping, an integrated analysis of Landsat-8 OLI data, aeromagnetic, geological and mineral indices maps was performed. Besides, aeromagnetics depicted a moderately fractured northern zone (the CAFB) contrasting with a high densely fractured zone (the CC, known as Ntem complex). The Ntem complex displays signatures of a meta-igneous, an intrusive complex, greenstone relics south of Sangmelima and hydrothermal activity. Together, these structures depict trans-compressions or trans-tensions corresponding to a broad NE-SW strike-slips channel that affect both the CAFB and the Ntem Complex, and they control the intrusions thus confirming a pervasive hydrothermal activity within the Ntem Complex. The proximity or coincidence of these porphyry centres with some mapped Iron-Gold affiliated mineral indices and porphyry granites indicate the possible occurrence of many hydrothermal ore deposits.
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dc.description.abstractThis essay discusses two early encounters of theater that took place in different parts of the world at approximately the same time: in the German-speaking countries in Europe and on the islands of Japan in Asia during the second half of the sixteenth century and the first decades of the seventeenth century. In both cases a particular kind of “national” theater emerged from these developments, which was able to embrace elements of highly diverse origins: Johann Wolfgang von Goethe’s Weimar theater plays and devices from different European performance cultures, and Izumo no Okuni’s kabuki elements stemming from a range of genres, including the Christian mystery plays. These new forms, recognized as a national theater, came into existence by way of intercultural performances. Ultimately, what came into being out of an “intercultural” encounter was later deemed genuinely “intracultural.”en
This study enhances the spatial resolution of TROPOMI HCHO and NO 2 columns by oversampling algorithms, and reduces the uncertainty of TROPOMI data. Study on ozone precursors in Beijing based on OLI and TROPOMI satellite data[J]. [9] Zhu L, Jacob D J, Mickley L J, et al. [23] Zhu L, Mickley L J, Jacob D J, et al. [35] Acdan J J M, Pierce R B, Dickens A F, et al.
Kobol unEle Kobol unobe. Nakai sesa habianiba kobol uno olaibbimo olebte kima bliba memei helasiba daamo ge dlakaibbua unino gibabiba damaiba yena gaa wembianiba eka yena naka un osa webinibbiobe. Ol man save raun long bus na kisim muruk kiau kam lukautim go na taim em buruk ol save wokim banis na putim pikinini muruk insait. Ol save givim ol kaikai go na taim ol kamap bikpla ol save kilim mumu na kaikai na tu long wokim sikan. Nau long displa taim tu oli save lukautim long kilim mumu na kaikai na kilim long salim na kisim moni.
