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Macerals of C1 Coal Seam in Parvade Coalfield (Tabas- Ira)

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@article{IJASEIT171,
   author = {Seyed Mohammad Hashemi},
   title = {Macerals of C1 Coal Seam in Parvade Coalfield (Tabas- Ira)},
   journal = {International Journal on Advanced Science, Engineering and Information Technology},
   volume = {2},
   number = {2},
   year = {2012},
   pages = {138--140},
   keywords = {Macerals ; Vitrinite; Ultraclarain; Parvade coalfield- Iran},
   abstract = {This paper deals with the study of the Late Triassic coal  deposits from Parvade coalfield in south of Tabas town and located geologically this is part of Central Iran zone. Coal main seam in Parvade coalfield named C1.Coals are rich in vitrinite, with average contents of 90%.Collinite is main part of vitrinite. their structures are homogenous .Telinite is low amount of vitrinite, based on ratio of collinite to telinite , subsidence of swamp is gradually and conditions  of environments is reduction and PH is acidic. Lithotype of coals is most ultraclarain with high amount of  vitrinite .some of amounts presents of semi-vitrinite and fusinite, micronite, skelerutinite and semi-fusinite macerals. High content of the vitrinite group macerals in these coals shows that water level was relatively high .Amount of vitrinite played key roles in coking.},
   issn = {2088-5334},
   publisher = {INSIGHT - Indonesian Society for Knowledge and Human Development},
   url = {http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=171},
   doi = {10.18517/ijaseit.2.2.171}
}

EndNote

%A Hashemi, Seyed Mohammad
%D 2012
%T Macerals of C1 Coal Seam in Parvade Coalfield (Tabas- Ira)
%B 2012
%9 Macerals ; Vitrinite; Ultraclarain; Parvade coalfield- Iran
%! Macerals of C1 Coal Seam in Parvade Coalfield (Tabas- Ira)
%K Macerals ; Vitrinite; Ultraclarain; Parvade coalfield- Iran
%X This paper deals with the study of the Late Triassic coal  deposits from Parvade coalfield in south of Tabas town and located geologically this is part of Central Iran zone. Coal main seam in Parvade coalfield named C1.Coals are rich in vitrinite, with average contents of 90%.Collinite is main part of vitrinite. their structures are homogenous .Telinite is low amount of vitrinite, based on ratio of collinite to telinite , subsidence of swamp is gradually and conditions  of environments is reduction and PH is acidic. Lithotype of coals is most ultraclarain with high amount of  vitrinite .some of amounts presents of semi-vitrinite and fusinite, micronite, skelerutinite and semi-fusinite macerals. High content of the vitrinite group macerals in these coals shows that water level was relatively high .Amount of vitrinite played key roles in coking.
%U http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=171
%R doi:10.18517/ijaseit.2.2.171
%J International Journal on Advanced Science, Engineering and Information Technology
%V 2
%N 2
%@ 2088-5334

IEEE

Seyed Mohammad Hashemi,"Macerals of C1 Coal Seam in Parvade Coalfield (Tabas- Ira)," International Journal on Advanced Science, Engineering and Information Technology, vol. 2, no. 2, pp. 138-140, 2012. [Online]. Available: http://dx.doi.org/10.18517/ijaseit.2.2.171.

RefMan/ProCite (RIS)

TY  - JOUR
AU  - Hashemi, Seyed Mohammad
PY  - 2012
TI  - Macerals of C1 Coal Seam in Parvade Coalfield (Tabas- Ira)
JF  - International Journal on Advanced Science, Engineering and Information Technology; Vol. 2 (2012) No. 2
Y2  - 2012
SP  - 138
EP  - 140
SN  - 2088-5334
PB  - INSIGHT - Indonesian Society for Knowledge and Human Development
KW  - Macerals ; Vitrinite; Ultraclarain; Parvade coalfield- Iran
N2  - This paper deals with the study of the Late Triassic coal  deposits from Parvade coalfield in south of Tabas town and located geologically this is part of Central Iran zone. Coal main seam in Parvade coalfield named C1.Coals are rich in vitrinite, with average contents of 90%.Collinite is main part of vitrinite. their structures are homogenous .Telinite is low amount of vitrinite, based on ratio of collinite to telinite , subsidence of swamp is gradually and conditions  of environments is reduction and PH is acidic. Lithotype of coals is most ultraclarain with high amount of  vitrinite .some of amounts presents of semi-vitrinite and fusinite, micronite, skelerutinite and semi-fusinite macerals. High content of the vitrinite group macerals in these coals shows that water level was relatively high .Amount of vitrinite played key roles in coking.
UR  - http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=171
DO  - 10.18517/ijaseit.2.2.171

RefWorks

RT Journal Article
ID 171
A1 Hashemi, Seyed Mohammad
T1 Macerals of C1 Coal Seam in Parvade Coalfield (Tabas- Ira)
JF International Journal on Advanced Science, Engineering and Information Technology
VO 2
IS 2
YR 2012
SP 138
OP 140
SN 2088-5334
PB INSIGHT - Indonesian Society for Knowledge and Human Development
K1 Macerals ; Vitrinite; Ultraclarain; Parvade coalfield- Iran
AB This paper deals with the study of the Late Triassic coal  deposits from Parvade coalfield in south of Tabas town and located geologically this is part of Central Iran zone. Coal main seam in Parvade coalfield named C1.Coals are rich in vitrinite, with average contents of 90%.Collinite is main part of vitrinite. their structures are homogenous .Telinite is low amount of vitrinite, based on ratio of collinite to telinite , subsidence of swamp is gradually and conditions  of environments is reduction and PH is acidic. Lithotype of coals is most ultraclarain with high amount of  vitrinite .some of amounts presents of semi-vitrinite and fusinite, micronite, skelerutinite and semi-fusinite macerals. High content of the vitrinite group macerals in these coals shows that water level was relatively high .Amount of vitrinite played key roles in coking.
LK http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=171
DO  - 10.18517/ijaseit.2.2.171