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KarstBase a bibliography database in karst and cave science.
Featured articles from Cave & Karst Science Journals
Characterization of minothems at Libiola (NW Italy): morphological, mineralogical, and geochemical study, Carbone Cristina; Dinelli Enrico; De Waele Jo
Chemistry and Karst, White, William B.
The karst paradigm: changes, trends and perspectives, Klimchouk, Alexander
Long-term erosion rate measurements in gypsum caves of Sorbas (SE Spain) by the Micro-Erosion Meter method, Sanna, Laura; De Waele, Jo; Calaforra, José Maria; Forti, Paolo
The use of damaged speleothems and in situ fault displacement monitoring to characterise active tectonic structures: an example from Zapadni Cave, Czech Republic , Briestensky, Milos; Stemberk, Josef; Rowberry, Matt D.;
Featured articles from other Geoscience Journals
Karst environment, Culver D.C.
Mushroom Speleothems: Stromatolites That Formed in the Absence of Phototrophs, Bontognali, Tomaso R.R.; D’Angeli Ilenia M.; Tisato, Nicola; Vasconcelos, Crisogono; Bernasconi, Stefano M.; Gonzales, Esteban R. G.; De Waele, Jo
Calculating flux to predict future cave radon concentrations, Rowberry, Matt; Marti, Xavi; Frontera, Carlos; Van De Wiel, Marco; Briestensky, Milos
Microbial mediation of complex subterranean mineral structures, Tirato, Nicola; Torriano, Stefano F.F;, Monteux, Sylvain; Sauro, Francesco; De Waele, Jo; Lavagna, Maria Luisa; D’Angeli, Ilenia Maria; Chailloux, Daniel; Renda, Michel; Eglinton, Timothy I.; Bontognali, Tomaso Renzo Rezio
Evidence of a plate-wide tectonic pressure pulse provided by extensometric monitoring in the Balkan Mountains (Bulgaria), Briestensky, Milos; Rowberry, Matt; Stemberk, Josef; Stefanov, Petar; Vozar, Jozef; Sebela, Stanka; Petro, Lubomir; Bella, Pavel; Gaal, Ludovit; Ormukov, Cholponbek;
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The Leading Edge, 2006, Vol 25, Issue 11, p. 1396-1400
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Prediction of a fracture-cavern system in a carbonate reservoir: A case study from Tahe oil field, China
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Guan Luping, Wang Shixing, Zhu Hailong,
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Abstract:
The carbonate reservoir in China's Tahe oil field is very heterogeneous with many caves and fractures that resulted from deposition, tectonic movements, diagenesis, and karstification. The reservoir spaces are mainly caves, pores, and fractures that resulted from karstification and structural deformation over several geologic periods. The Lower Ordovician carbonate rock, the main target, is at a depth of more than 5000 m. Karst topography dominates near the basal surface, fractures and caverns within the weathering zone. Laterally, the reservoirs are controlled by paleokarst highlands, slope, and faults that originated in different tectonic periods
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Keywords: carbonate, carbonate reservoir, carbonate rock, cavern, caves, china, deformation, deposition, depth, diagenesis, fault, faults, field, fracture, fractures, highlands, karst, karst topography, karstification, lower ordovician, movement, paleokarst, pores, prediction, reservoir, rock, slope, surface, system, weathering, zone,
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