Definition of palaeolatitude in English:

palaeolatitude

(US paleolatitude)

noun ˌpeɪlɪəʊˈlatɪtjuːdˌpalɪəʊˈlatɪtjuːdˌpālēōˈladət(y)o͞od

The latitude of a place at some time in the past, measured relative to the earth's magnetic poles in the same period. Differences between this and the present latitude are caused by continental drift and movement of the earth's magnetic poles.
Example sentencesExamples
- Fifth, much emphasis has been placed on paleomagnetic data indicating low depositional paleolatitudes.
- Palaeomagnetic data indicate that the palaeolatitude of the Atacama has been close to that of the present day since the late Jurassic.
- Of the lower plants, lycopods and horse-tails are rare whilst liverworts are abundant, particularly when compared to Cretaceous floras from lower palaeolatitudes.
- However, and very importantly, the distance from a palaeomagnetic pole and the sampled area of the continent, as reflected by palaeomagnetic inclination, provides a direct estimate of the palaeolatitude of the continent.
- Thus the sedimentological data indicating palaeolatitudes confirm the palaeomagnetic conclusions, in particular in the positioning of the South Pole under the Antarctic part of Gondwana.

Definition of paleolatitude in US English:

paleolatitude

nounˌpālēōˈladət(y)o͞od

The latitude of a place at some time in the past, measured relative to the earth's magnetic poles in the same period. Differences between this and the present latitude are caused by continental drift and movement of the earth's magnetic poles.
Example sentencesExamples
- Fifth, much emphasis has been placed on paleomagnetic data indicating low depositional paleolatitudes.
- Palaeomagnetic data indicate that the palaeolatitude of the Atacama has been close to that of the present day since the late Jurassic.
- However, and very importantly, the distance from a palaeomagnetic pole and the sampled area of the continent, as reflected by palaeomagnetic inclination, provides a direct estimate of the palaeolatitude of the continent.
- Of the lower plants, lycopods and horse-tails are rare whilst liverworts are abundant, particularly when compared to Cretaceous floras from lower palaeolatitudes.
- Thus the sedimentological data indicating palaeolatitudes confirm the palaeomagnetic conclusions, in particular in the positioning of the South Pole under the Antarctic part of Gondwana.

单词	palaeolatitude
释义	Definition of palaeolatitude in English: palaeolatitude (US paleolatitude) noun ˌpeɪlɪəʊˈlatɪtjuːdˌpalɪəʊˈlatɪtjuːdˌpālēōˈladət(y)o͞od The latitude of a place at some time in the past, measured relative to the earth's magnetic poles in the same period. Differences between this and the present latitude are caused by continental drift and movement of the earth's magnetic poles. Example sentencesExamples Fifth, much emphasis has been placed on paleomagnetic data indicating low depositional paleolatitudes. Palaeomagnetic data indicate that the palaeolatitude of the Atacama has been close to that of the present day since the late Jurassic. Of the lower plants, lycopods and horse-tails are rare whilst liverworts are abundant, particularly when compared to Cretaceous floras from lower palaeolatitudes. However, and very importantly, the distance from a palaeomagnetic pole and the sampled area of the continent, as reflected by palaeomagnetic inclination, provides a direct estimate of the palaeolatitude of the continent. Thus the sedimentological data indicating palaeolatitudes confirm the palaeomagnetic conclusions, in particular in the positioning of the South Pole under the Antarctic part of Gondwana. Definition of paleolatitude in US English: paleolatitude nounˌpālēōˈladət(y)o͞od The latitude of a place at some time in the past, measured relative to the earth's magnetic poles in the same period. Differences between this and the present latitude are caused by continental drift and movement of the earth's magnetic poles. Example sentencesExamples Fifth, much emphasis has been placed on paleomagnetic data indicating low depositional paleolatitudes. Palaeomagnetic data indicate that the palaeolatitude of the Atacama has been close to that of the present day since the late Jurassic. However, and very importantly, the distance from a palaeomagnetic pole and the sampled area of the continent, as reflected by palaeomagnetic inclination, provides a direct estimate of the palaeolatitude of the continent. Of the lower plants, lycopods and horse-tails are rare whilst liverworts are abundant, particularly when compared to Cretaceous floras from lower palaeolatitudes. Thus the sedimentological data indicating palaeolatitudes confirm the palaeomagnetic conclusions, in particular in the positioning of the South Pole under the Antarctic part of Gondwana.
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