RELATIONSHIP BETWEEN RIFT SPREADING AND LONGITUDINAL PROPAGATION RATES
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Aplonov S.V. | |
dc.date.accessioned | 2020-11-02T00:32:32Z | |
dc.date.available | 2020-11-02T00:32:32Z | |
dc.date.issued | 1990 | |
dc.identifier | https://elibrary.ru/item.asp?id=31155504 | |
dc.identifier.citation | Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 4, 82-86 | |
dc.identifier.issn | 0891-5571 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/18376 | |
dc.description.abstract | Work of recent years has convincingly shown that virtually all rift structures, whether continental or oceanic, expand in two directions simultaneously. Thus, the rift undergoes not only transverse extension (spreading), but also propagates, in a direction roughly perpendicular to the spreading, into the older lithosphere, breaking it up as the fault advances. Also, it is well known that the rates of these two components of expansion are not steady. We have analyzed rift generation in some regions where the evidence for advancement of oceanic rifts into continents in Recent or ancient times is strong. The rates of transverse extension (spreading) were estimated by the traditional approach, computing the distance between the pairs of identifiable magnetic anomalies of the same age. | |
dc.title | RELATIONSHIP BETWEEN RIFT SPREADING AND LONGITUDINAL PROPAGATION RATES | |
dc.type | Статья |
Files in this item
Files | Size | Format | View |
---|---|---|---|
There are no files associated with this item. |
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru