About This Item
- Full TextFull Text(subscription required)
- Pay-Per-View PurchasePay-Per-View
Purchase Options Explain
Share This Item
The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
Abstract
Pub. Id:
First Page:
Last Page:
Book Title:
Article/Chapter:
Subject Group:
Spec. Pub. Type:
Pub. Year:
Author(s):
Abstract:
The Carpathian Mountains formed during closure of the Tethys ocean during Cretaceous and Miocene convergent events. Three main shortening events occurred in the outer flysch Carpathians during Miocene time: (1) early Miocene events (old Styrian "phase," 18-20 Ma), (2) middle Miocene events (young Styrian "phase" ~ 15.5 Ma), and (3) late Miocene events (Moldavian "phase," 11-12 Ma). Early Miocene events include deformation and thrusting of the Pienides (Pieniny Klippen belt and Magura group nappes), en bloc overthrusting of the inner Dacides over the Pieniny Klippen belt, and thrusting within the most internal Moldavidian nappes (Audia-Czernahora, Macla, Convolute flysch, and Dukla(?) units). Middle Miocene events include thrusting within the Moldavidian nappes (Tarcau, Ma ginal Folds, Silesian, Skole, Subsilesian, and Waschberg units). Late Miocene events include thrusting within the outer Moldavidian nappes (Marginal Folds, Tarcau, Skole, Subsilesian, and Silesian units) and the Subcarpathian nappe. Minor Pliocene-Pleistocene folding occurred in the Subcarpathian nappe in the area of the southeast Carpathian bend. All of these Pienide and Moldavidian nappes consist only of sedimentary rocks, without their original crystalline basement. The westernmost limit of shortening migrated progressively eastward from one event to the next; in addition, shortening within each event may have occurred diachronously, being older in the west than in the east.
Pay-Per-View Purchase Options
The article is available through a document delivery service. Explain these Purchase Options.
Watermarked PDF Document: $14 | |
Open PDF Document: $24 |