Innovation and Integration: Exploration History, ExxonMobil, and the Guyana-Suriname Basin

2021 ◽  
Author(s):  
Audrey L. Varga ◽  
Matthew R. Chandler ◽  
Worth B. Cotton ◽  
Erik A. Jackson ◽  
Ross J. Markwort ◽  
...  

Abstract Exploration in the Guyana-Suriname Basin has been a decades-long endeavor, including technical challenges and a lengthy history of drilling with no offshore success prior to the Liza discovery. The 1929 New Nickerie well was the first onshore well in Suriname, and was followed by 30 years of dry holes before the heavy-oil Tambaredjo field was discovered in the 1960s. In the 1990s, nearly 40 years after the Tambaredjo discovery, ExxonMobil utilized the 1970s-vintage, poor-to moderate-quality, 2D seismic and gravity data available to create a series of hand-drawn, level-of-maturity (LOM) source and environments-of-deposition (EOD) maps over the basin to move their exploration efforts forward. This work established the genetic fundamentals necessary for understanding the hydrocarbon system and led to negotiation for and capture of the Stabroek Block in 1999. The Liza-1 success in 2015 spurred extensive activity in the Basin by ExxonMobil and the Stabroek Block co-venturers, Hess Guyana Exploration Limited and CNOOC Petroleum Guyana Limited (Austin et al. 2021). The collection of extensive state-of-the art seismic data has been leveraged to enable successful exploration of multiple play types across the Guyana-Suriname Basin. Further data collection, including over 2 km of conventional core and additional seismic data acquisition and processing, has enabled ExxonMobil to adopt interpretation techniques that are applied across the entire basin to characterize and understand the subsurface better. From initial hand-drawn maps to the use of advanced technology today, ExxonMobil's work in the Guyana-Suriname Basin has relied on integration of geologic and geophysical understanding as well as the ability to leverage new technology to continue a successful exploration program with 8 billion barrels discovered to date.

1999 ◽  
Vol 15 (1) ◽  
pp. 58-74 ◽  
Author(s):  
Madeleine MacMurraugh-Kavanagh ◽  
Stephen Lacey

It has long been the received wisdom that television drama has become increasingly ‘filmic’ in orientation, moving away from the ‘theatrical’ as its point of aesthetic reference. This development, which is associated with the rejection of the studio in favour of location shooting – made possible by the increased use of new technology in the 1960s – and with the adoption of cinematic as opposed to theatrical genres, is generally regarded as a sign that the medium has come into its own. By examining a key ‘moment of change’ in the history of television drama, the BBC ‘Wednesday Play’ series of 1964 to 1970, this article asks what was lost in the movement out of the studio and into the streets, and questions the notion that the transition from ‘theatre’ to ‘film’, in the wake of Ken Loach and Tony Garnett's experiments in all-film production, was without tension or contradiction. The discussion explores issues of dramatic space as well as of socio-cultural context, expectation, and audience, and incorporates detailed analyses of Nell Dunn's Up the Junction (1965) and David Mercer's Let's Murder Vivaldi (1968). Madeleine MacMurraugh-Kavanagh is the Post-Doctoral Research Fellow on the HEFCE-funded project, ‘The BBC Wednesday Plays and Post-War British Drama’, now in its third year at the University of Reading. Her publications include Peter Shaffer: Theatre and Drama (Macmillan, 1998), and papers in Screen, The British Journal of Canadian Studies, The Historical Journal of Film, Radio and Television, and Media, Culture, and Society. Stephen Lacey is a lecturer in Film and Drama at the University of Reading, where he is co-director of the ‘BBC Wednesday Plays’ project. His publications include British Realist Theatre: the New Wave and its Contexts (Routledge, 1995) and articles in New Theatre Quarterly and Studies in Theatre Production.


Author(s):  
William O'Brien

The Iberian Peninsula is one the most mineralized parts of Europe, with a long history of metal mining from prehistoric and Roman to modern times. The earliest evidence for copper metallurgy dates to the fifth millennium BC; however, distinctive Chalcolithic metalworking traditions did not emerge in most regions until 3000 BC onwards. There are widespread occurrences of copper mineralization in Spain and Portugal, including many areas with deposits of lead, tin, silver, and gold. Copper deposits occur in the Galician and Cantabrian mountain ranges of northern Spain, extending east to the Pyrenees. They are also numerous in central Spain, in the provinces of Madrid, Avila, Salamanca, and Segovia in the Central Range, and also in the Toledo and Betic mountains of Cordoba. Farther south, there are major copper deposits in the so-called Pyrite Belt, extending from Seville to Huelva into southern Portugal, and also in the Penibetic range from Cartagena to Malaga crossing the sierras of Almeria (Rovira 2002: fig. 3c; see Delibes de Castro and Montero Ruiz 1999 for regional surveys of copper deposits and indications of early mining; also Gómez Ramos 1999; Hunt Ortiz 2003). The widespread availability of ore deposits was a significant factor in the establishment of copper metallurgy in Iberia. How early is contentious, as is the means by which the new technology first developed in different parts of the peninsula. The older explanation of metal-seeking colonists from the east Mediterranean introducing this technology to southern Spain was replaced in the 1960s by a model that emphasized autonomous development (Renfrew 1967, 1973; Montero Ruiz 1994). This was based on the apparent antiquity of copper mining and metallurgy in Iberia and the distinctive technological processes that developed there relative to other parts of Europe. The earliest indication of copper metallurgy in Iberia may come from the settlement of Cerro Virtud in Almeria, south-west Spain. A single sherd from a metallurgical crucible used to reduce oxidized copper ore was discovered in a layer dated to the early fifth millennium BC (Montero Ruiz and Ruíz Taboada 1996; Ruíz Taboada and Montero Ruiz 1999).


2009 ◽  
Vol 62 (2) ◽  
pp. 277-288 ◽  
Author(s):  
Shigenobu Uraki ◽  
Yukari Kido ◽  
Yoshinori Sanada ◽  
Shin'ichi Kuramoto ◽  
Tadashi Okano ◽  
...  

2018 ◽  
Vol 58 (2) ◽  
pp. 773
Author(s):  
John Archer ◽  
Milos Delic ◽  
Frank Nicholson

Through a combination of innovative survey design, new technology and the introduction of novel operational techniques, the trace density of a 3D seismic survey in the Cooper Basin was increased from a baseline of 140 000 to 1 600 000 traces km–2, the bandwidth of the data was extended from four to six octaves, and the dataset was acquired in substantially the same time-frame and for the same cost as the baseline survey.


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