The the Middle Cretaceous-Lower Miocene petroleum system of the Kupal oil field, located in the Dezful Embayment has been studied. The Kazhdumi and Pabdeh are main source rocks, the Sarvak, Ilam and Asmari formations are reservoir and the Gachsaran formation is the seal rock. According to geochemical analysis the Kazhdumi and Pabdeh contributed to oil production and feeding the Asmari and Bange...

Homeland Security and Interoperability: Adding OGC Interfaces to ArcIMS & SDE Track: Homeland Security Author(s): Matthew Gentile Much of what we hope to achieve in Homeland Security is predicated on the notion that spatial data can flow freely (and securely) among government entities. The flow must occur on multiple axes, horizontally across jurisdictions, as well as vertically across levels f...

Imnaha Basalt and Grande Ronde Basalt (RI) of the Columbia River Basalt Group form a small synclinal basin immediately west of Riggins, Idaho. The displacement of the margins of the basalt outcrop, of the synclinal axis, and of a dike of Saddle Mountains(?) Basalt define a pattern best explained by a model of west-northwest to eastsoutheast and north-northwest to south-southeast dextral strike-...

Various evidence, including size and volume of the Siberian Traps, timing and duration of eruptions, paleotectonic and paleogeographic reconstructions, lithospheric structure, heat flow, trace element and radiogenic isotope compositions of lava are reviewed in this chapter. The major evidence may be summarized as follows. The Siberian Traps erupted in a number of brief volcanic events from the ...

The present study examines the imprint of salt tectonics on carbonate depositional patterns Ionian zone platform edge to slope transition. area is part an overturned rim syncline adjacent a diapir. made up three distinct stratigraphic sequences (pre-, syn- and post-rift sequences) represented by evaporites shallow water carbonates at base that pass gradually sequence consisting pelagic limeston...

The Western Syncline hosts reduced-facies, or Kupferschiefer-type, sedimentary rock-hosted stratiform Cu deposits (SSC) in the lowermost meters of Nonesuch Formation, which is part a thick section clastic rocks that comprise upper fill Mesoproterozoic Midcontinent Rift North America. Located Porcupine Mountains district Upper Peninsula, Michigan, these blind were discovered 1956, but are not ye...