Fluid Flow and Petroleum and Mineral Resources in the Upper (<20-km) Continental Crust

Author(s):  
Lawrence M. Cathles ◽  
Jennifer J. Adams
2020 ◽  
pp. jgs2020-116
Author(s):  
Jehiel Nteme Mukonzo ◽  
Marie-Christine Boiron ◽  
Yves Lagabrielle ◽  
Michel Cathelineau ◽  
Benoit Quesnel

The North Pyrenean Zone corresponds to the palaeopassive margin of the North Iberia plate, at the foot of which subcontinental mantle was exhumed during Albian times. Rare bodies of exhumed mantle rocks associated with strongly sheared lenses of continental crust are scattered among the North Pyrenean Zone metasediments. Significant fluid flow occurred along a major décollement at the basement–Trias interface in the Urdach massif (Chaînons Béarnais). Fluids with a broad range of salinity (10–38 wt.% NaCl equiv.), indicative of mixing between brines and more dilute waters, produced strong silicification of breccias. The brines circulated at c. 240–280°C under lithostatic pressures at c. 6 ± 1 km depth. The fluids became increasingly saline towards the final stages. The syndeposition of Cenomano-Turonian flysch layers then progressively isolated the lower aquifers close to the décollement where Triassic brines were predominant. The release and migration of significant volumes of brines during stretching and squeezing of the Triassic evaporites played a crucial part in the mineralogical and rheological transformations that occurred during the Pyrenean Cretaceous rifting event.


2017 ◽  
Vol 10 (9) ◽  
pp. 685-690 ◽  
Author(s):  
Oliver Plümper ◽  
Alexandru Botan ◽  
Catharina Los ◽  
Yang Liu ◽  
Anders Malthe-Sørenssen ◽  
...  

Geology ◽  
1997 ◽  
Vol 25 (1) ◽  
pp. 15 ◽  
Author(s):  
Eric Pili ◽  
Simon M. F. Sheppard ◽  
Jean-Marc Lardeaux ◽  
Jean-Emmanuel Martelat ◽  
Christian Nicollet

2018 ◽  
Vol 12 (1) ◽  
pp. 80-80
Author(s):  
Oliver Plümper ◽  
Alexandru Botan ◽  
Catharina Los ◽  
Yang Liu ◽  
Anders Malthe-Sørenssen ◽  
...  

2015 ◽  
Vol 31 (4) ◽  
pp. 151-160
Author(s):  
Tadeusz Piecuch ◽  
Jacek Piekarski ◽  
Łukasz Gajewski

Abstract The study presents the method of determining constant coefficient b2, occurring in general filtration equation (1), in the second part of the denominator, that is in the expression for deposit resistance In the considerations, lack of the deposit’s compressibility was assumed, which means that the deposit porosity is constant. With such an assumption, constant coefficient b2 is equivalent with transmission coefficient, which occurs in commonly known and accepted equation – as the baseline equation – for fluid flow through a porous layer according to Darcy (Piecuch 2009, 2010). This study is another publication in the cycle of basic tests of the filtration process which constitute next publications of the authors, published in Rocznik Ochrona Środowiska [Annual Set the Environmental Protection] as well as in the magazine Gospodarka Surowcami Mineralnymi [Mineral Resources Management], to which the reader interested in these problems can refer. Another study will be the publication discussing the filtration process with the creation of sediment on the filtration deposit, hence in the general filtration equation (1) the value of sediment resistance RO will appear in the denominator. Relevant cycle of publications will study the possibilities of use of gravitational deposit filters in which the porous deposit will be the set of coal grains, while the fed mixture will also be the post-production suspension of coal grains.


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