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Detailed interpretations of reflection seismic data and new U-Pb and Hf isotope geochemistry in zircon, reveal that the basement of the Lower Magdalena Valley basin is the northward continuation of the basement terranes of the northern Central Cordillera, and thus that the Lower Magdalena experienced a similar pre-Cenozoic tectonic history as the latter.
Detailed interpretations of aerial photographs clearly reveal fault scarps at Ban Mai, Ban Don Fai, and Ban Samai Nuea ((A) and (C) in Fig. 4).
Detailed interpretations of aerial photographs reveal fault scarps at Ban Mai, Ban Don Fai, and Ban Samai Nuea ((A) and (C) in Fig. 4), and reveal the following six geometrical fault segments along the southeastern margin of the Lampang Basin: Ban Don Fai, Ban Mai, Ban Mae Ip, Doi Ton Ngun, Mae Than, and Sop Prap (Fig. 1(B)).
Detailed interpretations of qualitative findings from the study communities are discussed elsewhere (Flint et al. 2010).
Based on [the] limited evidence about the stratigraphy and its relationship to the fossils, it is premature to make detailed interpretations about the site formation processes.
Full results and detailed interpretations are provided in the accompanying supplementary material.
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Detailed interpretation of those signals by targeted LC/MS2 analysis revealed four groups of compounds.
Detailed interpretation of these analyses reveals the reservoirs internal thin shale architecture, and the presence of gas chimneys.
However, in practice, the low signal-to-noise ratio of the ET datasets precludes detailed interpretation and makes their assessment difficult.
Detailed interpretation and mapping of multi-channel seismic reflection profiles from the Adana Basin show that a south-verging linked imbricate thrust stack existed across the northern portion of the Adana Basin prior to the deposition of early Miocene sedimentary successions.
Detailed interpretation of single channel seismic reflection and Huntec deep-tow boomer and sparker profiles demonstrates that the southwestern Black Sea shelf formed by a protracted shelf-edge progradation since the Miocene Pliocene.
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