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SSRN Electronic Journal, 2012 This paper arose out of discussions that took place during sessions of the Fourth Perm Economic Forum. A theme-based event, the Forum is held annually every September. In 2008, the theme of the Forum was urban development, including, naturally, development strategies for the city as a regional capital.
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Journal of Asian Earth Sciences, 2002
Abstract Permo-Triassic carbonates with minor basal clastics cover extensive tracts of the Shan Plateau in the eastern part of Myanmar. These carbonates are grouped into the Permian Thitsipin Limestone Formation and the Late Permian–Early Triassic Nwabangyi Dolomite Formation.
Nyunt Htay, Thura Oo, Tin Hlaing
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Abstract Permo-Triassic carbonates with minor basal clastics cover extensive tracts of the Shan Plateau in the eastern part of Myanmar. These carbonates are grouped into the Permian Thitsipin Limestone Formation and the Late Permian–Early Triassic Nwabangyi Dolomite Formation.
Nyunt Htay, Thura Oo, Tin Hlaing
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The composition of Permian seawater
Geochimica et Cosmochimica Acta, 1991Forty-nine brine inclusions in marine halite from the Ochoan Salado Formation in the Delaware Basin and fifteen inclusions in halite from the Leonardian Wellington Formation in the Kansas Basin were extracted, and their chemical compositions were determined.
Thomas J. Friedman +3 more
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, 1995 The first question concerning the Permian of China is, “Where in the world…?” Agreement is general that China consists of a maze of blocks or terranes, amalgamated along complex sutures and fold belts (Fig. 1). There is, understandably, considerably less agreement on where they originated and their history of amalgamation (Table 1).
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Upper Permian Stratigraphy of West Texas Permian Basin [PDF]
AAPG Bulletin, 1935 By comparing the Upper Permian stratigraphy of West Texas and Oklahoma it is found that the Whitehorse of Oklahoma is equivalent to the lower evaporites of the southern basin and that the Permian of the Oklahoma Quartermaster is equivalent to the Yates sand. Formations above the Yates in the southern basin are younger than any of the Oklahoma or Kansas
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AAPG Bulletin, 1925
The general geographic provinces of India are named, the formations are shown in a table, the permian formations are briefly described, the presence of coal is noted, the widespread glaciation indicated, and the possibility of oil in the Permian discussed.
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The general geographic provinces of India are named, the formations are shown in a table, the permian formations are briefly described, the presence of coal is noted, the widespread glaciation indicated, and the possibility of oil in the Permian discussed.
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The Biostratigraphy of Permian Palynofloras
Proceedings of the Annual Meeting. American Association of Stratigraphic Palynologists, 1970Abstract Classical paleobotanical theory separates the floras of the Permian Period into four distinctive provinces: (1) the Gondwanian; (2) the Angaran; (3) the Ca‐thaysian; and (4) the Euramerican. These floras are based on the stem and leaf remains which are the chief preservable macroscopic parts of plants.
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Geological Society, London, Special Publications, 1964
Summary Twelve rocks for which calculated isotopic ages are mutually consistent and for which there is some biostratigraphic control have been used in the construction of a Permian time-scale. On the evidence of these rocks it is suggested that the Permian period lasted from about 280 m.y to about 225 m.y.
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Summary Twelve rocks for which calculated isotopic ages are mutually consistent and for which there is some biostratigraphic control have been used in the construction of a Permian time-scale. On the evidence of these rocks it is suggested that the Permian period lasted from about 280 m.y to about 225 m.y.
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1995
The Permian of Pakistan has been well known, yet poorly understood. Pakistan represents one of the few places where the Permian of the Paleotethys (Northern Hemisphere) and the Permian of Gondwana both occur. This chapter will review the stratigraphy of Pakistan that represents the northern part of the Indian/Pakistan plate.
Kevin R. Pogue, Bruce R. Wardlaw
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The Permian of Pakistan has been well known, yet poorly understood. Pakistan represents one of the few places where the Permian of the Paleotethys (Northern Hemisphere) and the Permian of Gondwana both occur. This chapter will review the stratigraphy of Pakistan that represents the northern part of the Indian/Pakistan plate.
Kevin R. Pogue, Bruce R. Wardlaw
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Revision of the stratigraphy of Permian and supposed Permian rocks of Southern Scotland
Geologische Rundschau, 1978The formal stratigraphy of the Permian basins of southern Scotland is described for the first time. These rocks consist of piedmont breccias and lavas, overlain by wadi-fan and dune complexes, and alluvial fan and floodplain sediments. The sequences are inferred to be Stephanian to Lower Permian in age and correlatable with similar continental ...
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