Comparison of deeply buried paleoregolith profiles, Norwegian North Sea, with outcrops from southern Sweden and Georgia, USA Implications for petroleum exploration

被引:18
作者
Riber, Lars [1 ]
Dypvik, Henning [1 ]
Sorlie, Ronald [2 ]
Naqvi, Syed Asmar Aal-E-Muhammad [1 ]
Stangvik, Kristian [1 ]
Oberhardt, Nikolas [1 ]
Schroeder, Paul A. [3 ]
机构
[1] Univ Oslo, Dept Geosci, POB 1047, N-0316 Oslo, Norway
[2] Lundin Norway AS, Strandveien 4, N-1366 Lysaker, Norway
[3] Univ Georgia, Dept Geol, Athens, GA 30602 USA
关键词
Paleoregolith; Mesozoic weathering; Utsira High; North Sea; Petroleum reservoir; Surface paleoregolith; WEATHERING PROFILES; KAOLIN MINERALS; QUARTZ DIORITE; DEPTH TRENDS; CLAY; SOIL; SAPROLITE; POROSITY; REGOLITH; GRANITE;
D O I
10.1016/j.palaeo.2017.01.043
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
For the first time on the Norwegian Continental Shelf, deeply buried paleoregolith profiles have been identified as part of the petroleum reservoirs in recently discovered oil fields on the Utsira High, Norwegian North Sea. Reservoir properties (porosity and permeability) in the granitic basement on the Utsira High are mainly the result of physical and chemical alteration of the rock occurring in the near-surface environment during sub-aerial exposure of the high in the Mesozoic. Evaluating the reservoir potential of altered basement rocks requires a different approach than in conventional petroleum exploration. In this paper, macroscopic, mineralogical and micromorphological alteration features observed in two deeply buried paleoregolith profiles are compared with surface paleoregoliths from No Klack, Sweden and Georgia, USA. The paleoregolith profiles are subdivided into specific weathering fades (altered coherent rock fades, saprock facies and saprolite facies) based on the rock fabric and mechanical strength. The reservoir potential of each weathering facies is controlled by the type and degree of alteration. In the altered coherent rock fades, porosity and permeability is mainly controlled by joints and microfractures that developed prior to subaerial exposure of the granitic pluton. In the saprock fades, intensified chemical dissolution of plagioclase enhanced porosity and the development of mesofractures improved the connectivity between pores. In the saprolite facies, progressive dissolution of plagioclase creates porosity, but the precipitation of clays within voids and mesofractures has a destructive effect on the overall reservoir properties. The deeply buried paleoregolith profiles from the Utsira High display comparable macroscopic, mineralogical and micromorphological alteration features to what was observed in surface paleoregoliths from No Klack and Georgia. Outcrop studies may therefore be an important tool when evaluating the reservoir potential in subsurface paleoregoliths. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:82 / 95
页数:14
相关论文
共 121 条
[1]   Late Jurassic to earliest Cretaceous palaeoclimatic evolution of the southern North Sea [J].
Abbink, O ;
Targarona, J ;
Brinkhuis, H ;
Visscher, H .
GLOBAL AND PLANETARY CHANGE, 2001, 30 (3-4) :231-256
[2]   THE VANGA GRANITE, SOUTH SWEDEN - A COMPLEX GRANITIC INTRUSION [J].
ABERG, G ;
KORNFALT, KA ;
NORD, AG .
GEOLOGISKA FORENINGENS I STOCKHOLM FORHANDLINGAR, 1985, 107 :153-159
[3]   THE DEVELOPMENT OF CRYSTALLINE BASEMENT AQUIFERS IN A TROPICAL ENVIRONMENT [J].
ACWORTH, RI .
QUARTERLY JOURNAL OF ENGINEERING GEOLOGY, 1987, 20 (04) :265-272
[4]   Triassic-Jurassic weathering and clay mineral dispersal in basement areas and sedimentary basins of southern Sweden [J].
Ahlberg, A ;
Olsson, I ;
Simkevicius, P .
SEDIMENTARY GEOLOGY, 2003, 161 (1-2) :15-29
[5]  
[Anonymous], 2006, FRONTIERS EXPLORATIO
[6]  
[Anonymous], 3 INT GEOM C 23 28 A
[7]  
[Anonymous], 2005, Clays
[8]  
[Anonymous], 2001, SOILS INTRO PALEOPED
[9]  
Asbjornsen E., 2015, THESIS
[10]  
Bahlburg H, 2011, GEOL SOC MEM, V36, P81, DOI 10.1144/M36.6