scholarly journals Comparison of seismic processing and interpretation tradeoffs between Kirchoff and finite-difference migrations, using poststack migrated data in the west Niger Delta, Nigeria

2013 ◽  
Vol 4 (3) ◽  
pp. 272-276
Author(s):  
Etim Uko ◽  
Chibuogwu Eze
1977 ◽  
Vol 18 (1) ◽  
pp. 1-19 ◽  
Author(s):  
David Henige

The flowering of the Atlantic trade in the seventeenth and eighteenth centuries caused many of the West African societies of the near hinterland to orient themselves increasingly toward the coast. This new focus created new geopolitical conformations. Given the nature of the stimulus, trade and politics went hand in hand and entrepreneurial ability could reap political rewards. These possibilities were greatest along the Gold Coast and in the Niger delta where the actual European presence was small in relation to the extent of the trade.Such a trader cum political leader was John Kabes who, in a career spanning nearly forty years, established the paramount stool of Komenda, hitherto part of the inland state of Eguafo. Kabes began as a trader for the English (and sometimes for the Dutch) and gradually achieved political status which, however it may have been acquired, proved to be lasting because it was acceptable to existing political mores.Such of Kabes's activities as are known suggest that his success sprang from his ability to wring advantage from the new exigencies of the time and place in ways which enabled him to acquire legitimacy as well as wealth and influence. Although Kabes's career is uniquely documented there is no reason to suppose that it was particularly unusual in its other facets. On this argument it can suggest ways in which other West African trade-derived polities, particularly in the Niger delta, may have coalesced.


Author(s):  
I. V. Mikhaylov ◽  
D. V. Velesov ◽  
V. N. Glinskikh

On the example of the Priobskoye oil field of the West Siberian oil and gas province, we show the relevance of studying thin-layered oil-saturated reservoirs, as well as consider the corresponding world experience. The operating principle of a probe system with toroidal sources and receivers is described, after which we perform 2D finite-difference simulation and analysis of its signals in typical geoelectric reservoir models. The dependence of the signals on the resistivity anisotropy coefficient is demonstrated. In realistic geoelectric sections of the Priobskoye field, obtained by numerical inversion of BKZ field data, 2D finite-difference simulation for the system with toroids is conducted. It implies the fundamental possibility of investigating thin-layered electrically anisotropic deposits of the Priobskoye field by means of the system with toroidal sources and receivers.


2002 ◽  
Vol 21 (12) ◽  
pp. 1227-1231
Author(s):  
William A. Schneider ◽  
Paul Docherty ◽  
Mike Plumlee

1974 ◽  
Vol 15 (4) ◽  
pp. 563-585 ◽  
Author(s):  
Paul E. Lovejoy

Only recently have historians devoted much attention to monetary developments in African history, primarily because the substantivist school of economic anthropology, which has argued that so-called western economic theory does not apply to African situations, has dominated the field. This view has been increasingly under attack in recent years, particularly by a new group of economic historians who have found many aspects of formal economic theory useful in the reconstruction of Africa's past. Marion Johnson's pioneering work on the gold mithqal and cowrie shell, for example, has documented the spread of a common currency over much of West Africa, throughout an area encompassed by Lake Chad in the east, the upper reaches of the Senegambia in the west, the southern Sahara in the north, and the region between the Volta basin and the Niger Delta in the south. The study of other currencies, including the copper rod standard of the Cross River basin in Nigeria and Cameroons, and the cloth money of the Senegambia, has demonstrated the importance of other standards besides cowries and gold, so that it is now known that virtually all of precolonial West Africa had economies sufficiently developed to require the use of circulating mediums of exchange and units of account. This breakthrough raises a number of important questions which seriously challenge, if not completely undermine, the predominant view that Africa's past, down to very recent times, has been subsistence oriented, non-market directed, and basically static.


2021 ◽  
Author(s):  
Laure Schenini ◽  
Alexandra Skrubej ◽  
Mireille Laigle ◽  
Alessandra Ribodetti ◽  
Laure Combe ◽  
...  

<p>Offshore 2D-Multichannel seismic (MCS)-reflection profiles were acquired in northern Ecuador during the HIPER survey (March/April 2020, R/V L’Atalante) together with one 2D-OBS-seismic-refraction profile (presented in a joint abstract by A. Skrubej). This project (presented in a joint abstract by A. Galve) aims at deciphering the role of lower plate structural heterogeneities and fluids on subduction zone seismogenesis processes within the 2016 Pedernales rupture segment, which is characterized by contrasting slip behaviors. We put a particular emphasis on the segment located at the northern termination of the subducting Carnegie Ridge which was devoid of previous seismic investigations. Three lines of 315-km-long in total, one North of the 2016 Pedernales rupture zone sampling an area experiencing aseismic slip and two lines parallel to the trench, were recorded using an airgun source of 4990 in<sup>3</sup> and a 6-km-long streamer. In this study, we present in detail the seismic processing workflow used to produce an enhanced imaging of the Ecuadorian margin, a prerequisite for tackling the project’s objectives.</p><p>We performed routine MCS data processing onboard to produce post-stack time migrated sections using Geovation<sup>® </sup>CGG’s software. The dip-line collected across the northern Atacames seamounts area provides a detailed image through the whole Nazca oceanic crust down to the Moho, showing a normal crust thickness, at least on the oceanward portion, up to 15 km to the west of the trench. At the trench, we image a horst-like basement topographic high, which outcrops at sea-bottom, offsets the deformation front arcwards, with the outcropping frontal decollement reflector topping this oceanic basement high. Its nature, fluid content potential and lateral extent need to be determined, but its observation at the shallow portion of the interplate megathrust contribute to expand the inventory of subducting rough structures possibly impacting the megathrust frictional slip behavior.</p><p>Further advanced processing include noise attenuation, 2D-SRME multiple attenuation, Kirchhoff pre-stack time migration and preserved amplitude pre-stack depth migration (PSDM) performed in the angle domain. The megathrust fault located at the top of the subducting oceanic crust is imaged down to 7 km depth at a distance of 28 km from the trench which will contribute to complement the high-resolution version of the slab’s top topography close to the trench. A joint analyze of this MCS line and the coincident 2D-OBS-refraction Vp model, reveal that variations in moho acoustic features at 15 km distance to the west of the trench correlates with a 30 km wide and >10-km-thick low Vp anomaly. Nearby previous experiment SISTEUR seismic lines are being reprocessed using the same workflow, in order to further investigate the deep crustal seismic structures over the Pedernales 2016 rupture zone.</p>


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