The timing of salt structure growth in the Southern Permian Basin (Central Europe) and implications for basin dynamics

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F19%3A00507723" target="_blank" >RIV/67985530:_____/19:00507723 - isvavai.cz</a>

Výsledek na webu

<a href="https://onlinelibrary.wiley.com/doi/abs/10.1111/bre.12323" target="_blank" >https://onlinelibrary.wiley.com/doi/abs/10.1111/bre.12323</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1111/bre.12323" target="_blank" >10.1111/bre.12323</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The timing of salt structure growth in the Southern Permian Basin (Central Europe) and implications for basin dynamics

Popis výsledku v původním jazyce

In this paper, a literature-based compilation of the timing and history of salt tectonics in the Southern Permian Basin (Central Europe) is presented. The tectono-stratigraphic evolution of the Southern Permian Basin is influenced by salt movement and the structural development of various types of salt structures. The compilation presented here was used to characterize the following syndepositional growth stages of the salt structures: (a) “phase of initiation”, (b) phase of fastest growth (“main activity”), and (c) phase of burial. We have also mapped the spatial pattern of potential mechanisms that triggered the initiation of salt structures over the area studied and summarized them for distinct regions (sub-basins, platforms, etc.). The data base compiled and the set of maps produced from it provide a detailed overview of the spatial and temporal distribution of salt tectonic activity enabling the correlation of tectonic phases between specific regions of the entire Southern Permian Basin. Accordingly, salt movements were initiated in deeply subsided graben structures and fault zones during the Early and Middle Triassic. In these areas, salt structures reached their phase of main activity already during the Late Triassic or the Jurassic and were mostly buried during the Early Cretaceous. Salt structures in less subsided sub-basins and platform regions of the Southern Permian Basin mostly started to grow during the Late Triassic. The subsequent phase of main activity of these salt structures took place from the Late Cretaceous to the Cenozoic. The analysis of the trigger mechanisms revealed that most salt structures were initiated by large-offset normal faults in the sub-salt basement in the large graben structures and minor normal faulting associated with thin-skinned extension in the less subsided basin parts.

Název v anglickém jazyce

The timing of salt structure growth in the Southern Permian Basin (Central Europe) and implications for basin dynamics

Popis výsledku anglicky

In this paper, a literature-based compilation of the timing and history of salt tectonics in the Southern Permian Basin (Central Europe) is presented. The tectono-stratigraphic evolution of the Southern Permian Basin is influenced by salt movement and the structural development of various types of salt structures. The compilation presented here was used to characterize the following syndepositional growth stages of the salt structures: (a) “phase of initiation”, (b) phase of fastest growth (“main activity”), and (c) phase of burial. We have also mapped the spatial pattern of potential mechanisms that triggered the initiation of salt structures over the area studied and summarized them for distinct regions (sub-basins, platforms, etc.). The data base compiled and the set of maps produced from it provide a detailed overview of the spatial and temporal distribution of salt tectonic activity enabling the correlation of tectonic phases between specific regions of the entire Southern Permian Basin. Accordingly, salt movements were initiated in deeply subsided graben structures and fault zones during the Early and Middle Triassic. In these areas, salt structures reached their phase of main activity already during the Late Triassic or the Jurassic and were mostly buried during the Early Cretaceous. Salt structures in less subsided sub-basins and platform regions of the Southern Permian Basin mostly started to grow during the Late Triassic. The subsequent phase of main activity of these salt structures took place from the Late Cretaceous to the Cenozoic. The analysis of the trigger mechanisms revealed that most salt structures were initiated by large-offset normal faults in the sub-salt basement in the large graben structures and minor normal faulting associated with thin-skinned extension in the less subsided basin parts.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2019

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Basin Research

ISSN

0950-091X

e-ISSN

—

Svazek periodika

31

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

24

Strana od-do

337-360

Kód UT WoS článku

000461051800007

EID výsledku v databázi Scopus

2-s2.0-85057765685