Journal of Ear Printed in Chi https://doi.org Dey, J., Sen, S Journal of Ear Sequ F 1. Coal In 2. Ge AB dl in re ta ph ci Fo co LA fa to th gr K tio 0 INTRODU Sequence a process orie tional system space and tim geography. Se lated strata, b conformities. sequence strat mation, a maj ranpura Coal west trending Core holes ha mentary struct The facies ass been correlate Interpretations been integrate and deposition Gondwana suc *Correspondin © China Univ Germany, Part Manuscript rec Manuscript ac rth Science, Vo ina /10.1007/s1258 S., 2018. Seque rth Science, 29( uence St Formatio ndia Limited, Ce eologix Limited Joyjit Dey: htt BSTRACT: G le Permian Ba n a normal fau esistivity-densi ation. Core stu hysical logs an es analysis has our major fini ommodation sy AST is charac acies, while floo o meandering d he western par raben setting. KEY WORDS: on. UCTION e stratigraphy is ented stratigraph and stratal sta me on a basin s equence stratig bounded by un The objective tigraphic mode jor economic c Field, a wester Damodar Valle ave been studie tures and infer t semblages, infe ed to the avail s from cores a ed to decipher s nal model of t ccession (Damo ng author: souv versity of Geosc t of Springer N ceived March 2 ccepted April 12 l. 29, No. 4, p. 83-018-0791-7 nce Stratigraph (4): 745–754. ht tratigra on from entral Mine Pla , Dynasty Build tps://orcid.org/0 Gondwana depo arakar Format ult setting. Av ty from drilled udy identifies nd modeled fie s been used to ing upward de ystem tract (L cterized by ver odplain domin depositional sy rt, supported b fluvial sequen s a methodolog hic framework acking pattern/a scale as well as graphy studies nconformities o of this study el of Middle Pe coal-bearing un rnmost membe ey Basin, easter ed in detail to i the possible dep erred from the able geophysic as well as geo sedimentary arc the Barakar Fo odar Valley Bas vikseniitb@gma ciences and Spr ature 2018 24, 2018. 2, 2018. 745–754, Augu hic Model of M ttps://doi.org/10 aphic M m a Mar Joyjit De anning and Des ding, Level-4, W 0000-0002-2149 osits are exten tion from the m vailability of e d wells) from t fluvial sedime ld-wide to und establish a seq epositional sequ LAST) at base rtically stacke nated facies ch ystem from bot by eastward th nce stratigraph gy/tool that prov to interpret dep architecture thr s reconstruct p the genetically or their correl was to deciph ermian Barakar nit of the North er of the large rn Gondwana, I investigate the positional proce e core analysis, cal logs field w ophysical logs chitectural elem ormation of ea sin), which then ail.com ringer-Verlag G ust 2018 iddle Permian B 0.1007/s12583- Model of rginal G ey 1 , Souvik sign Institute (C Wing-A, Andher 9-2054; Souv sively found a marginal Gond extensive cores he study area entary architec derstand vertic quence stratigr uences were id e and high ac ed, multistory haracterizes HA ttom to top of hinning of sed hy, Gondwana vides posi- ough aleo- y re- lative her a r for- h Ka- east- ndia. sedi- esses. , had wide. have ments astern n has GmbH been Stud opp mod drill 1 G Gon nort form Jhar dire area the Kar a w Vall bear tecto havi and spre Jhar thick Low Barakar Format 018-0791-7. htt f Middl Gondwa k Sen * 2 CMPDI), Region ri Kurla Road, A vik Sen: https:// cross the conti dwana Basin, s as well as ge helped us achi ctures, which cal and horizo raphic model o dentified, each ccommodation amalgamated AST, reflecting each cycle. Stu iment packets sediment, Mid n used to const dy from this ea ortunity to est del integrating led wells, yieldi GEOLOGY OF Karanpura Co ndwana basins th-west of Ran ms part of Ran rkhand State. I ction and 75 k a of about 2 28 area into Nort anpura Coal Fi westernmost par ley Basin (Fig ring Lower Go onic trough (ap ing a maximum a width of ab eads over Haz rkhand State, In Stratigraphy o k sedimentary s wer to Middle tion from a Ma tp://en.earth-sc e Perm ana Bas nal Institute-3, J Andheri (E), Mu /orcid.org/0000 inents. Here w eastern India, eophysical log ieving high res were correlat ontal facies dis of the cyclic Ba sequence com n system tract channel sand g a gradual sh udy reveals dep , all being dep ddle Permian, truct a fluvial s stern Gondwan tablish the reg core and geoph ing greater degr F THE STUDY oal Field, one in India Penin nchi and 20 km nchi, Hazariba It extends for km in east-wes 80 km 2 . The As th Karanpura C eld (SKF). The rt of the vast g. 1), constitut ondwana sedim pprox. 1 230 km m length of 64 bout 36 km in zaribagh, Ranc ndia (Priyadarsh of the North Ka succession from Gondwana Gro IS arginal Gondwa ience.net ian Bar sin, Ind Jharkhand 829 umbai 400 059, 0-0002-2796-47 we study the M , being deposit g suites (gamm solution interp ed with the ge sposition. The arakar depositi mprises of low a (HAST) at to dstone dominat hift from braid pocenter to be posited in a ha Barakar Form sequence strati na Basin provid gional sequenc hysical logs fro ree of confiden Y AREA e of the major sular is situate m south-west o agh and Palam about 38 km st direction en shwa Pahar hil Coal Field (NK e North Karanp east-west chai tes a large exp ments deposited m 2 ). It is a sauce km in the east the north-south hi and Palama hi, 2004). aranpura Coal F m Carboniferou oup of rocks fr SSN 1674-487X ana Basin, India rakar ia 103, India , India 737 Mid- ted ma- re- eo- fa- ion. ac- op. ted ded e in alf- ma- graphic model. des an excellent ce stratigraphic om hundreds of nce. r coal bearing d about 60 km of Hazaribagh, mau districts of in north-south compassing an l ranges divide KF) and South pura Coal Field, in of Damodar panse of coal- d mostly in the er shaped basin, t-west direction h direction and au districts of Field consists of s to Cretaceous rom Talchir to X a. . t c f g m , f h n e h , r - e , n d f f s; o