释义 |
Definition of syncline in English: synclinenounˈsɪŋklʌɪnˈsɪnˌklaɪn Geology A trough or fold of stratified rock in which the strata slope upwards from the axis. Compare with anticline Example sentencesExamples - A series of transverse anticlines and synclines are observed that have axes orientated NE-SW, approximately perpendicular to the fault zone.
- The faults have a systematic geometric relationship with folds, with anticlines in the mutual hanging walls of fault pairs and broader footwall synclines that define the shallow dish forms of the polygons.
- Complex folding makes detailed interpretations of the geological structure difficult, but the area essentially consists of a large, tightly folded syncline that strikes about N.20 [degrees] E.
- A series of synclines and anticlines developed within the basin at several localities but most prominently south of the Aghios Georgios fault zone.
- At several localities a west-verging footwall syncline has developed as a consequence of westward transport on the overlying thrust sheet.
Origin Late 19th century: from syn- 'together' + Greek klinein 'to lean', on the pattern of incline. Definition of syncline in US English: synclinenounˈsɪnˌklaɪnˈsinˌklīn Geology A trough or fold of stratified rock in which the strata slope upward from the axis. Compare with anticline Example sentencesExamples - A series of transverse anticlines and synclines are observed that have axes orientated NE-SW, approximately perpendicular to the fault zone.
- At several localities a west-verging footwall syncline has developed as a consequence of westward transport on the overlying thrust sheet.
- The faults have a systematic geometric relationship with folds, with anticlines in the mutual hanging walls of fault pairs and broader footwall synclines that define the shallow dish forms of the polygons.
- A series of synclines and anticlines developed within the basin at several localities but most prominently south of the Aghios Georgios fault zone.
- Complex folding makes detailed interpretations of the geological structure difficult, but the area essentially consists of a large, tightly folded syncline that strikes about N.20 [degrees] E.
Origin Late 19th century: from syn- ‘together’ + Greek klinein ‘to lean’, on the pattern of incline. |