Structural Diagenesis, Early Embrittlement and Fracture Setting in Shallow-Water Platform Carbonates (Monte Alpi Southern Apennines, Italy)

2019 ◽  
Author(s):  
V. La Bruna ◽  
J. Lamarche ◽  
F. Agosta ◽  
A. Rustichelli ◽  
A. Giuffrida ◽  
...  
Keyword(s):  
Shallow Water ◽  
Southern Apennines ◽  
Platform Carbonates

A MULTIDISCIPLINARY APPROACH TO GLOBAL CORRELATION AND GEOCHRONOLOGY. THE CRETACEOUS SHALLOW-WATER CARBONATES OF SOUTHERN APENNINES, ITALY

2004 ◽  
pp. 103-122 ◽  
Author(s):  
BRUNO D’ARGENIO ◽  
VITTORIA FERRERI ◽  
HELMUT WEISSERT ◽  
SABRINA AMODIO ◽  
FRANCESCO P. BUONOCUNTO ◽  
...  
Keyword(s):  
Shallow Water ◽  
Multidisciplinary Approach ◽  
Southern Apennines ◽  
Global Correlation

A record of global change: OAE 1a in Dariyan shallow-water platform carbonates, southern Tethys, Persian Gulf, Iran

Facies ◽  
2016 ◽  
Vol 62 (4) ◽  
Author(s):  
Mehrangiz Naderi-Khujin ◽  
Ali Seyrafian ◽  
Hossein Vaziri-Moghaddam ◽  
Vahid Tavakoli
Keyword(s):  
Global Change ◽  
Shallow Water ◽  
Persian Gulf ◽  
Platform Carbonates ◽  
Southern Tethys

Silica diagenesis in Eocene shallow-water platform carbonates, southern Pyrenees

Sedimentology ◽  
1999 ◽  
Vol 46 (6) ◽  
pp. 969-984 ◽  
Author(s):  
Jordi Gimenez-Montsant ◽  
Francesc Calvet ◽  
Maurice E. Tucker
Keyword(s):  
Shallow Water ◽  
Silica Diagenesis ◽  
Platform Carbonates

Palaeogeographic Significance of Clay Mineral Distributions in the Inferior Oolite Group (Mid Jurassic) of Southern England

Clay Minerals ◽  
1989 ◽  
Vol 24 (1) ◽  
pp. 91-105 ◽  
Author(s):  
L. E. Jones ◽  
B. W. Sellwood
Keyword(s):  
Shallow Water ◽  
Clay Mineral ◽  
Mixed Layer ◽  
Southern England ◽  
Mineral Assemblages ◽  
Platform Carbonates ◽  
Basinal Facies

AbstractFive areally distinct mineral assemblages are recognized in the Inferior Oolite of S. England. In each area, vertical (stratigraphic) variations are insignificant. The five assemblages comprise varying proportions of illite, illite-smectite, kaolinite, chlorite and kaolinite-smectite, the mixed-layer clays being largely poorly crystalline and randomly interstratified. A predominantly detrital rather than authigenic origin is suggested for most of the clays. Shallow-water platform carbonates contain kaolinite with illite and illite-smectite. Kaolinite decreases in abundance away from former mid-Jurassic land areas, the deeper shelf and more basinal facies being dominated by illite and/or illite-smectite. Possible volcanic contributions to clay suites are suggested but cannot yet be fully evaluated. The palaeogeographic usefulness of clay mineral suites is confirmed, even in carbonate-dominated systems.

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