Middle Permian (Wordian) Mixed Boreal—Tethyan Brachiopod Fauna from Matsukawa, South Kitakami Belt, Japan

Tazawa, Jun-ichi; Araki, Hideo

doi:10.2517/2016pr029

Cited by 2 publications

(3 citation statements)

References 46 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…found in Gua Belong, Gua Senurat, Gua Henderik, Gua Batu Tinggi, and Merapoh suggests deposition within the photic zone (Fontaine et al, 1995;Abdullah & Rahman, 1995). In general, fossil assemblages in the northern Central Belt correlates with other regional warm Paleo-Tethys fauna such as the Lengwu fauna of South China (Liang, 1990) and Kitakami Mountains of Japan (Tazawa et al, 2000).…”

Section: Depositional Environment Andmentioning

confidence: 98%

“…Diagnostic fossils which serve as index fossils and age determinants were found within formations of interest are listed in Table 2. The signature Upper Permian Paleofusulina -Colaniella -Reichelina zone of Central Belt Peninsular Malaysia (Abdullah & Rahman, 1995) correlates with those in north Thailand (Sakagami & Hatta, 1982), Cambodia (Ishii et al, 1969), Kitakami Mountain of Japan (Tazawa et al, 2000), and the Lengwu fauna of South China (Liang, 1990). These regions harbor Paleotethys/Tethys realm fauna, signifying the warm tropical region during the Permo-Triassic.…”

Section: Paleontologymentioning

confidence: 99%

See 1 more Smart Citation

The Gua Musang Group: A newly proposed stratigraphic unit for the Permo-Triassic sequence of Northern Central Belt, Peninsular Malaysi

Mohamed¹,

Joeharry

Leman³

et al. 2016

BGSM

View full text Add to dashboard Cite

The close association between the Gua Musang formation, Telong formation, Aring Formation, and Nilam marble reflect the lateral facies changes among these formations. Poorly delineated boundaries between each formation calls for a reassessment on the genetic and stratigraphic correlation of these formations. The newly proposed Gua Musang Group is defined as argillite-carbonate-volcanic deposited within the same Gua Musang platform during Permo-Triassic period, which includes all four formations under study. High resolution stratigraphy is needed for each formation for better stratigraphic correlation between the various lithostratigraphic units of the Gua Musang Group and other chronologically related rock formations in the region.The new division of formations within this Group is proposed based on lithologies and stratigraphic correlation that could provide better understanding on the geology of northern section of Central Belt of Peninsular Malaysia.

show abstract

Section: Depositional Environment Andmentioning

confidence: 98%

Section: Paleontologymentioning

confidence: 99%

The Gua Musang Group: A newly proposed stratigraphic unit for the Permo-Triassic sequence of Northern Central Belt, Peninsular Malaysi

Mohamed¹,

Joeharry

Leman³

et al. 2016

BGSM

View full text Add to dashboard Cite

show abstract

“…1;Minato and Kato, 1970, figs. 4-7 -Asama, 1967, 1981Asama and Murata, 1974Cathaysiopteris Psygmophyllum Taeniopteris , 1988 Taeniopteris Asama and Murata, 1974 Huang and Chen Hayasaka, 1926Hayasaka, , 1933, 1932Minato, 1949a, b;Tazawa et al, 2010bTazawa et al, , 2012bTazawa et al, , 2016b 8 9 Tazawa and Takakuwa, 2009;Tazawa et al, 2012a12 12 Shen et al, 201112 13 Tazawa and Shen, 1997 Enteletes gibbosus 1 Tazawa, 1998 6 6 , 1919;Hayasaka, 1932;Tazawa et al, 1998;Shen et al, 1999Shen et al, , 2006Tomida, 2000 11 14 Yanagida andHirata, 1969 Tazawa and Shen 1997 Shen et al, 2011;Tazawa et al, 1998, 2016b-Tazawa et al, 2016b , 1900;Hayasaka, 1917Hayasaka, , 1922aHayasaka, , b, 1925Hayasaka, , 1937Hayasaka, , 1953Hayasaka, , 1960Hayasaka, , 1963Hayasaka, , 1964Hayasaka, , 1966Hayasaka, , 1967Minato, 1955;Hayasaka and Minato, 1956;Minato and Nakamura, 1956;Nakamura, 1959bNakamura, , 1960…”

Section: Tachibana 1981b Athyris Takozuensis a Sulcifera 1956mentioning

confidence: 99%

Palaeobiogeographical studies on the Palaeozoic brachiopods of Japan, and their tectonic significance: A review

Tazawa

2018

Jour. Geol. Soc. Japan

Self Cite

View full text Add to dashboard Cite

We reviewed studies (based mainly on brachiopods) of the Palaeozoic biogeography of Japan. The data indicate four tectonic events:) during the Silurian-Permian, Proto-Japan was located within the Central Asian Orogenic Belt, near North China;) after the late Permian, Proto-Japan was rearranged through large-scale, sinistral strike-slip faulting, probably during the Early Cretaceous to Palaeogene;) Akiyoshi-type limestone basalt blocks were derived from early Carboniferous to middle Permian reef-seamounts in the northern Panthalassa, near Proto-Japan; and) Mino-type limestone-basalt blocks were derived from late Carboniferous to late Permian reef-seamounts in the equatorial Panthalassa, near North America (Texas).

show abstract

Middle Permian (Wordian) Mixed Boreal—Tethyan Brachiopod Fauna from Matsukawa, South Kitakami Belt, Japan

Cited by 2 publications

References 46 publications

The Gua Musang Group: A newly proposed stratigraphic unit for the Permo-Triassic sequence of Northern Central Belt, Peninsular Malaysi

The Gua Musang Group: A newly proposed stratigraphic unit for the Permo-Triassic sequence of Northern Central Belt, Peninsular Malaysi

Palaeobiogeographical studies on the Palaeozoic brachiopods of Japan, and their tectonic significance: A review

Contact Info

Product

Resources

About