Structurally controlled hydrothermal dolomite (HTD) reservoir facies and associated
productive leached limestones are major hydrocarbon producers in North America and are …

Aesthetically appealing thrust systems and related large-scale anticlines, in both active and
fossil foreland fold-and-thrust belts, and the economic potential associated with them, have …

Abstract Sediment-hosted Pb-Zn deposits can be divided into two major subtypes. The first
subtype is clastic-dominated lead-zinc (CD Pb-Zn) ores, which are hosted in shale …

The four‐part districting scheme (wedge‐top, foredeep, forebulge, and backbulge
depozones) applies to many foreland basin systems worldwide, but significant variations …

Passive margins have existed somewhere on Earth almost continually since 2740 Ma. They
were abundant at 1900–1890, 610–520, and 150–0 Ma, scarce at ca. 2445–2300, 1600 …

Paleontologic and stratigraphic evidence points to the early Paleozoic Precordilleran terrane
of western Argentina as being the conjugate rift pair of the Appalachians. Stratigraphic …

To test the suitability of using shale geochemistry as a provenance indicator of a source with
an ultramafic component, we used ICP Mass Spectrometry to analyze 130 samples from …

Remarkable advances in age dating Mississippi Valley-type (MVT) lead–zinc deposits
provide a new opportunity to understand how and where these deposits form in the Earth's …

Sedimentologic, petrographic, and U‐Pb detrital zircon ages from middle Eocene through
early Miocene sedimentary rocks in the Lesser Himalayan zone of western and central …

The evolution of Oman's onshore sedimentary basins from the Late Precambrian to the
Present is reflected by six tectono-stratigraphic units. Unit I, the Precambrian basement …