scholarly journals Geophysical log characterization of the Flamborough Chalk Formation (Late Cretaceous, Santonian – Early Campanian), East Yorkshire, UK: implications for understanding the onshore and offshore occurrence of the Late Campanian Rowe Chalk Formation

2018 ◽  
Vol 62 (3) ◽  
pp. 201-209 ◽  
Author(s):  
M. A. Woods
2021 ◽  
Vol 40 (11) ◽  
pp. 823-830
Author(s):  
Nikita Bondarenko ◽  
Sherilyn Williams-Stroud ◽  
Jared Freiburg ◽  
Roman Makhnenko

Carbon sequestration activities are increasing in a global effort to mitigate the effects of greenhouse gas emissions on the climate. Injection of wastewater and oil-field fluids is known to induce seismic activity. This makes it important to understand how that risk relates to CO2 injection. Injection of supercritical CO2 into the Cambrian Mt. Simon sandstone in Illinois Basin induced microseismicity that was observed below the reservoir, primarily in the Precambrian crystalline basement. Geomechanical and flow properties of rock samples from the involved formations were measured in the laboratory and compared with geophysical log data and petrographic analysis. The controlling factors for induced microseismicity in the basement seem to be the hydraulic connection between the reservoir and basement rock and reactivation of pre-existing faults or fractures in the basement. Additionally, the presence of a laterally continuous low-permeability layer between reservoir and basement may have prevented downward migration of pore pressure and reactivation of critically stressed planes of weakness in the basement. Results of the geomechanical characterization of this intermediate layer indicate that it may act as an effective barrier for fluid penetration into the basement and that induced microseismicity is likely to be controlled by the pre-existing system of faults. This is because the intact material is not expected to fail under the reservoir stress conditions.


2021 ◽  
Vol 14 (18) ◽  
Author(s):  
Neetu Mohan ◽  
Sugumar Vasudevan ◽  
Paramasivam Chellamuthu Ranganathan ◽  
Anandhan Narayanasamy

2014 ◽  
Vol 1618 ◽  
pp. 169-180 ◽  
Author(s):  
Francisco Riquelme ◽  
José Luis Ruvalcaba-Sil ◽  
Jesús Alvarado-Ortega ◽  
Emilio Estrada-Ruiz ◽  
Martin Galicia-Chávez ◽  
...  

ABSTRACTCoahuilite, a new variety of amber is described from the Late Cretaceous Olmos Formation (ca. 73 Ma.), Coahuila, north of México. This amber is totally distinct chemically and stratigraphically from the Miocene Chiapas amber (ca. 23-13 Ma.), Southern México, which according to mineral nomenclature is currently known as Simojovelite var. nov. Additionally, an emended description of Bacalite is proposed, based on the physicochemical analysis and geological record of a fossil resin recently recovery from the Late Cretaceous El Gallo Formation (ca. 73 Ma.), Baja California, northwestern México. The results are supported by characterization of such ambers using synchrotron-based Infrared (FTIR) microspectroscopy.


2016 ◽  
Vol 457 ◽  
pp. 221-232 ◽  
Author(s):  
Júlio C. de A. Marsola ◽  
Alessandro Batezelli ◽  
Felipe C. Montefeltro ◽  
Gerald Grellet-Tinner ◽  
Max C. Langer
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