Matches in SemOpenAlex for { <https://semopenalex.org/work/W1566571114> ?p ?o ?g. }
Showing items 1 to 81 of
81
with 100 items per page.
- W1566571114 abstract "A detailed hydrogeologic model of the liquid-dominated Cerro Prieto geothermal field in Mexico (located in Baja California about 35 km (22 mi) south of the US border) has been developed to identify subsurface geothermal fluid flow paths. Two different methods were used to define the geologic model of the Cerro Prieto field. In the first, the lithology was divided into seven different formations based on correlatable groups of beds having distinct lithologic, structural, and fluid production characteristics. In the second method, the lithology was classified into three basic types of lithofacies: shales, sandy shales, and sands. Faults identified by the first method were incorporated into lithofacies sections. Hot fluids are believed to enter the field at depths greater than 3000 m (10,000 ft) from the east through a thick, porous sand unit, called Sand Unit Z, which dips gently to the east. This unit underlies a 450 to 600 m (1500 to 2000 ft) thick low porosity shale unit, named Shale Unit 0, which acts as a local caprock. The fluids flow westward until they encounter a normal fault, Fault H, with downthrow to the southeast. The fluids then move up along this fault until they again encounter Sand Unitmore » Z along the upthrown side of Fault H. Whereas most of the fluids continue to flow westward through Sand Unit Z, a small portion rise along Fault H. The westward flow continues until it reaches a gap in the overlying Shale Unit O. There, some of the flow rises up and into the western Shale Unit 0, which is sandier in this region, while the rest continues to flow westward through Sand Unit Z. Eventually, some of the geothermal fluids leak to the surface, whereas the rest mix with colder waters that surround the geothermal system.« less" @default.
- W1566571114 created "2016-06-24" @default.
- W1566571114 creator A5013796967 @default.
- W1566571114 creator A5025033192 @default.
- W1566571114 creator A5067564355 @default.
- W1566571114 date "1983-03-01" @default.
- W1566571114 modified "2023-09-26" @default.
- W1566571114 title "Geologic and geothermal fluid flow models of Cerro Prieto field" @default.
- W1566571114 hasPublicationYear "1983" @default.
- W1566571114 type Work @default.
- W1566571114 sameAs 1566571114 @default.
- W1566571114 citedByCount "0" @default.
- W1566571114 crossrefType "journal-article" @default.
- W1566571114 hasAuthorship W1566571114A5013796967 @default.
- W1566571114 hasAuthorship W1566571114A5025033192 @default.
- W1566571114 hasAuthorship W1566571114A5067564355 @default.
- W1566571114 hasConcept C111766609 @default.
- W1566571114 hasConcept C114793014 @default.
- W1566571114 hasConcept C121332964 @default.
- W1566571114 hasConcept C122792734 @default.
- W1566571114 hasConcept C127313418 @default.
- W1566571114 hasConcept C151730666 @default.
- W1566571114 hasConcept C153127940 @default.
- W1566571114 hasConcept C165205528 @default.
- W1566571114 hasConcept C17409809 @default.
- W1566571114 hasConcept C175551986 @default.
- W1566571114 hasConcept C187320778 @default.
- W1566571114 hasConcept C2778887201 @default.
- W1566571114 hasConcept C33556824 @default.
- W1566571114 hasConcept C48258643 @default.
- W1566571114 hasConcept C57879066 @default.
- W1566571114 hasConcept C5900021 @default.
- W1566571114 hasConcept C6494504 @default.
- W1566571114 hasConcept C8058405 @default.
- W1566571114 hasConcept C90278072 @default.
- W1566571114 hasConceptScore W1566571114C111766609 @default.
- W1566571114 hasConceptScore W1566571114C114793014 @default.
- W1566571114 hasConceptScore W1566571114C121332964 @default.
- W1566571114 hasConceptScore W1566571114C122792734 @default.
- W1566571114 hasConceptScore W1566571114C127313418 @default.
- W1566571114 hasConceptScore W1566571114C151730666 @default.
- W1566571114 hasConceptScore W1566571114C153127940 @default.
- W1566571114 hasConceptScore W1566571114C165205528 @default.
- W1566571114 hasConceptScore W1566571114C17409809 @default.
- W1566571114 hasConceptScore W1566571114C175551986 @default.
- W1566571114 hasConceptScore W1566571114C187320778 @default.
- W1566571114 hasConceptScore W1566571114C2778887201 @default.
- W1566571114 hasConceptScore W1566571114C33556824 @default.
- W1566571114 hasConceptScore W1566571114C48258643 @default.
- W1566571114 hasConceptScore W1566571114C57879066 @default.
- W1566571114 hasConceptScore W1566571114C5900021 @default.
- W1566571114 hasConceptScore W1566571114C6494504 @default.
- W1566571114 hasConceptScore W1566571114C8058405 @default.
- W1566571114 hasConceptScore W1566571114C90278072 @default.
- W1566571114 hasLocation W15665711141 @default.
- W1566571114 hasOpenAccess W1566571114 @default.
- W1566571114 hasPrimaryLocation W15665711141 @default.
- W1566571114 hasRelatedWork W1495597890 @default.
- W1566571114 hasRelatedWork W1497399097 @default.
- W1566571114 hasRelatedWork W1503372535 @default.
- W1566571114 hasRelatedWork W1517422592 @default.
- W1566571114 hasRelatedWork W1604903288 @default.
- W1566571114 hasRelatedWork W1644016943 @default.
- W1566571114 hasRelatedWork W2002631544 @default.
- W1566571114 hasRelatedWork W2045255442 @default.
- W1566571114 hasRelatedWork W2056624785 @default.
- W1566571114 hasRelatedWork W2114879407 @default.
- W1566571114 hasRelatedWork W2151864114 @default.
- W1566571114 hasRelatedWork W2280364368 @default.
- W1566571114 hasRelatedWork W2297966282 @default.
- W1566571114 hasRelatedWork W2537006084 @default.
- W1566571114 hasRelatedWork W2555958719 @default.
- W1566571114 hasRelatedWork W2788282533 @default.
- W1566571114 hasRelatedWork W3035456531 @default.
- W1566571114 hasRelatedWork W316882280 @default.
- W1566571114 hasRelatedWork W59098982 @default.
- W1566571114 hasRelatedWork W88701795 @default.
- W1566571114 isParatext "false" @default.
- W1566571114 isRetracted "false" @default.
- W1566571114 magId "1566571114" @default.
- W1566571114 workType "article" @default.