The development of the Mianyang-Changning intracratonic sag significantly influenced the
Late Proterozoic to Early Cambrian oil/gas occurrences in the Sichuan basin, that is, chiefly through its influence on the distribution of high-quality reservoirs in the
Late Proterozoic Dengying and Early Cambrian Longwangmiao formations and of source-rocks in the Niutitang Formation.
Late Proterozoic rocks of Nagar Parkar, southeastern Pakistan: A preliminary petrologic account, In: Ahmed, R.
Late Proterozoic and Silurian alkaline plutons within the southeastern New England Avalon zone.
By that time the transgressive sea environment was not yet entirely developed, but the sedimentation environment of the
Late Proterozoic had already faded.
The southern Appalachian Blue Ridge is composed predominantly of
late Proterozoic metaclastic and metavolcanic units overprinted by a mid-Paleozoic dynamothermal event that recrystallized these units to a range of metamorphic grades.
It has always been thought that the Earth completely froze twice during the
late Proterozoic era between 600 and 800million years ago.
The Pampean cycle developed during the
Late Proterozoic. It shows a collisional heft at the easternmost part of the Sierras Pampeanas, with a series of mafic and ultramafic rocks associated with tectonites.
Basement exposures in southwestern Rhode Island are dominated by multiply deformed
late Proterozoic to late Paleozoic plutonic and metasedimentary rocks [ILLUSTRATION FOR FIGURE 1 OMITTED].
Then sometime during the
late Proterozoic era, about 580 million years ago, life got big.
The Nagar Parkar Igneous Complex (NPIC) is considered as an extension of the
Late Proterozoic Malani Igneous suite (MIS) of western Rajasthan.