Distribution and Origin of Natural Gas Leakage Features on Block 2 of the Orange Basin as Interpreted from 2D Seismic Reflection Data Off-shore the South African Margin.

2009 ◽  
Author(s):  
Donna Boyd ◽  
Z. Anka ◽  
R.di Primio ◽  
Maarten de Wit ◽  
Jeff Aldrich
Keyword(s):  
Natural Gas ◽  
South African ◽  
Seismic Reflection ◽  
The South ◽  
Seismic Reflection Data ◽  
Gas Leakage ◽  
Reflection Data ◽  
Origin Of Natural Gas

New insights into the structure of the South Caspian Basin from seismic reflection data, Gorgan Plain, Iran

2018 ◽  
Vol 108 (2) ◽  
pp. 379-402 ◽  
Author(s):  
Ali Radfar ◽  
Aziz Rahimi Chakdel ◽  
Ali Nejati ◽  
Mehrdad Soleimani ◽  
FaridTaati
Keyword(s):  
Seismic Reflection ◽  
Caspian Basin ◽  
The South ◽  
South Caspian Basin ◽  
Seismic Reflection Data ◽  
Reflection Data

Proterozoic deformation beneath Banks Island: implications for the regional extent of the Racklan orogeny

1990 ◽  
Vol 27 (4) ◽  
pp. 605-613
Author(s):  
Frederick A. Cook
Keyword(s):  
Relative Position ◽  
Seismic Reflection ◽  
The South ◽  
Arctic Canada ◽  
Seismic Reflection Data ◽  
Thrust Faulting ◽  
Reflection Data ◽  
Banks Island ◽  
Mackenzie Mountains ◽  
Northeast Corner

Seismic reflection data from the northeast corner of Banks Island in arctic Canada show that Proterozoic layers were subjected to at least two deformational events prior to the Cambrian. The oldest of these events involved folding and faulting(?) from west-northwest to east-southeast. The ages of the layers that were subjected to this deformation are unknown; however, younger Proterozoic layers, probably correlative with the Shaler Group (ca. 1.1–0.8 Ga), unconformably overlie the folded and faulted layers, and were themselves regionally arched prior to the Cambrian. The relative position of the oldest deformed strata is thus the same as that of the strata observed to the south beneath the Anderson Plains, where thrust faulting and folding deformed pre-Mackenzie Mountains Supergroup (Shaler Group equivalent) layers during at the time of the Racklan orogeny (ca. 1.1–1.2 Ga). Distant effects of the Racklan orogeny may therefore extend to at least the northeast side of Banks Island.

The style of transverse faulting in the Dead Sea basin from seismic reflection data: The Amazyahu fault

2006 ◽  
Vol 55 (3) ◽  
pp. 129-139 ◽  
Author(s):  
Avihu Ginzburg ◽  
Moshe Reshef ◽  
Zvi Ben-Avraham ◽  
Uri Schattner
Keyword(s):  
Seismic Reflection ◽  
Dead Sea ◽  
Seismic Reflection Data ◽  
Reflection Data ◽  
Dead Sea Basin ◽  
The Dead

Archive of digital boomer seismic reflection data collected offshore east-central Florida during USGS cruise 00FGS01, July 14-22, 2000

Data Series ◽  
10.3133/ds496 ◽  
2009 ◽  
Author(s):  
Janice A. Subino ◽  
Shawn V. Dadisman ◽  
Dana S. Wiese ◽  
Karynna Calderon ◽  
Daniel C. Phelps
Keyword(s):  
Seismic Reflection ◽  
Seismic Reflection Data ◽  
East Central ◽  
Central Florida ◽  
Reflection Data
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