Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Holger C. Forke"'
Autor:
Holger C. Forke, Stanko Buser
Publikováno v:
Geologija, Vol 37/38, Pp 153-171 (1995)
The first conodont fauna (4 species) from the "Trogkofel Limestones" of the Karavanke Mts. (Dolžanova soteska) is described and correlated with the fusulinids(3 species) within the same sample. The occurrence of Streptognathodus cf. simplex, Strepto
Externí odkaz:
https://doaj.org/article/4dcbee3cc06f467ab25450e14cd8946d
Publikováno v:
GeoArabia. 17:59-104
The upper part of the Saiq and lower part of the Mahil formations in the Oman Mountains represent outcrop time-equivalents to the highly prolific, hydrocarbon-bearing subsurface Middle and Upper members of the Khuff Formation (K4-K1 reservoir interva
Publikováno v:
GeoArabia. 17:85-128
The investigated Middle to Upper Triassic Upper Mahil Member, representing a Jilh outcrop equivalent in the Northern Oman Mountains, illustrates the proximal portion of a flat epeiric carbonate ramp. A sedimentological study of well-exposed outcrops
Autor:
Michael Obermaier, Bastian Koehrer, Thomas Aigner, Christoph J. Schneider, Michael Poppelreiter, Holger C. Forke
Publikováno v:
GeoArabia. 16:69-108
The Lower Triassic Sudair Formation represents the deposits of an epeiric carbonate-evaporite-siliciclastic platform. It is widely known as top seal for the underlying Khuff reservoir in some of the largest hydrocarbon accumulations in the world (e.g
Autor:
Michael Zeller, Suleiman Al-Kindi, Bastian Koehrer, Thomas Aigner, Paul Milroy, Holger C. Forke, Michael Poeppelreiter
Publikováno v:
Scopus-Elsevier
The Middle Permian to Lower Triassic Khuff Formation is one of the most important reservoir intervals in the Middle East. This study presents a sequence stratigraphic analysis of the Khuff Formation of a well-exposed outcrop in the Oman Mountains, wh
Autor:
Carlos A. Méndez, Darwin R. Boardman, Beate Fohrer, Lance L. Lambert, Holger C. Forke, Elisa Villa, Alexandra V. Djenchuraeva, Olga L. Kossovaya, María Luisa Martínez-Chacón, Luis C. Sánchez de Posada, Svetlana Remizova, N.V. Goreva, Greg Wahlman, James E. Barrick, Aleksander S. Alekseev, Elias Samankassou, T.N. Isakova, Philip H. Heckel, Tamara I. Nemyrovska, Katsumi Ueno, David M. Work
Publikováno v:
Palaeoworld. 18:114-119
Studies carried out for more than 10 years by the Task Group to establish GSSPs at the base of the Moscovian–Kasimovian and Kasimovian–Gzhelian boundaries have resulted in the proposal that the level at which the conodont species Idiognathodus si
Publikováno v:
Facies. 51:541-553
Silicified schwagerinids (superfamily Fusulinoidea v. Moeller 1878) from the Upper Carboniferous (Carnic Alps, Austria and Italy) were isolated from cemented carbonate rocks using hydrochloric acid. The shells show details of the wall texture and of
Autor:
Holger C. Forke
Publikováno v:
Facies. 47:201-275
In order to establish a refined biostratigraphic subdivision and correlation of the Uppermost Carboniferous/Lower Permian deposits of the Southern Alps (Carnic Alps, Karavanke Mountains; Austria/Italy/Slovenia), two major microfossil groups (fusulino
Autor:
Elias Samankassou, Holger C. Forke
Publikováno v:
Facies. 42:177-210
The fusulinacean faunal content of the Bombaso Fm. and lower part of the Auernig Group (Carnic Alps, Austria/Italy) is reviewed and completed by data on conodonts and algae. Four different faunal associations can be distinguished within this stratigr
Publikováno v:
Senckenbergiana lethaea. 78:1-39
The Lower “Pseudoschwagerina” Limestone (Rattendorf Group) is a cyclic sequence composed of fossiliferous, shallow marine limestones and thin clastic beds. In the Schulterkofel section three depositional cycles are well developed. Clastic interva