Journal of Ear Printed in Chi https://doi.org Mendhe, V. A with Implicati http://en.earth- Organ of J Vinod A D 2. II 4. AB stu se ra ev ir te to m an tia va ca ef cu co K 0 INTRODU In the rec to provide am resources defi from shale ga and advances hydraulic frac et al., 2015; L 2007; Montgo natural gas (m shales. Shales posed of main erals, especial (Varma et al. generated from *Correspondin © China Univ Germany 2017 Manuscript rec Manuscript ac rth Science, Vo ina /10.1007/s1258 A., Mishra, S., K ions to Shale G -science.net no-Petro Jharia B Atmaram M Durgesh Kum 1. T (ISM)-Depar . IIT (ISM)-Dep BSTRACT: T udies indicate ervoir characte akar shale bed vident that Ba regular hair-li errestrial-fluvia o 17.32 wt.%, i matter ranging nd 74.74 vol.% ated that Bara alues of the sur apacity, this is ffect. The pore urve with the ombined-slit an KEY WORDS: UCTION cent years, sha mple of hydroca icit. Increased as reservoirs is obtained in h turing technolo Loucks et al., 2 omery et al., 20 mostly methan s are fine grain nly clay matters lly quartz/mica ., 2015; Hardy m the transform ng author: vame versity of Geosc 7 ceived April 11 ccepted June 24 l. 28, No. 5, p. 8 83-017-0779-8 Khangar, R. G., Gas Reservoir. ograph Basin wi Mendhe * 1 , S mar 1 , Atul K CSIR-Central I tment of Chemi 3. GSI-Geolog partment of App Vinod A The shale depo their potentia eristics are stil ds of eastern p rakar shales a ine fractures a atile deposits u indicating goo from 0.28 vol % to 99.10 vol.% akar shales are rface area dete because of dia e size distribut H2 type of h nd bottle neck shale gas, petr ale gas has beco arbon to balanc growth of natu due to the suc horizontal drilli ogies (Shiver et 2009; Jarvie et 005; Curtis, 20 ne) obtains fro ned, clastic sedi s and tiny fragm a and 2%–20% y, 2014; Brow mation of organ endhe@gmail.c ciences and Spr 1, 2017. , 2017. 897–916, Octob et al., 2017. Or Journal of Ea ic and P ith Imp Subhashree M Kumar Varm Institute of Min ical Engineerin gical Survey of I plied Geology, I Atmaram Mendh osits of Damod al for shale gas ll rare in India part of Jharia are carbonaceo and showing li under reducin d source rock l.% to 12.98 v %, respectively e vitrinite rich ermined follow agenesis and a tion signifying hysteresis patte pores. rographic com ome very impo ce the convent ural gas produ ccessful applic ing and multi-s t al., 2015; Wa al., 2007; Polla 002). Shale gas m organically imentary rock c ments of other % of organic m wn, 2009). Met nic matter by b com ringer-Verlag G ber 2017 rgano-Petrogra arth Science, 2 Pore Fa plication Mishra 1 , Ra ma 4 , H. Singh ing and Fuel Re ng, Indian Instit India, Central R Indian Institute he: http://orcid. dar Valley hav . However, fun a, as exploratio Basin are eval ous, silty, cont ithological var g environment potentiality. T ol.%, 0.17 vol y. The ternary h and placed in wing different alterations of p g the micro to ern, specifies position, surfa ortant ional ction ation stage ang L astro, s is a rich com- min- matter thane bacte- GmbH rial proc 2010 tem main accu ess reso shal spon micr clay Cha depe matu (Me 200 sour 26 s karo cont Peri aphic and Pore F 8(5): 897–916. acets of ns to Sh njit G. Khan h 1 , Sujeet Ku esearch, Dhanb tute of Technolo Region, Nagpur e of Technology .org/0000-0003 ve received gre ndamental info on is in the pr luated for gas tains sub-angu riations along t. The values o The vitrinite, l l.% to 3.23 vol y facies plot of n the thermal- methods point potash feldspar mesoporous n the heterogen ace area, pore d action (biogen cesses during t 0; Claypool, 19 where it acts nly methane an umulation (Jarv of adsorption ource for the re le gas system nsible for the i ropore structure y minerals (Va almers and Bus ends on their th urity, depth and endhe et al., 20 8). In India, s rce of energy. T sedimentary ba o, Cambay, G taining thick s iod (Padhy and Facets of Permi https://doi.org Permia hale Gas ngar 3 , Alka D mar 1 , Mollik bad 826 015, In ogy (ISM), Dha r 440 006, India y (ISM), Dhanba -3212-8298 eat attention s ormation allied rimary stage. I reservoir cha ular flecks of q the bedding p of TOC varies iptinite, inerti l.%, 0.23 vol.% f maceral comp -dry gas prone t towards low r responsible f nature, while T neity in pore s disposition, po nic gas) and ge the burial at v 998). Shales ar as both source nd is the store h vie et al., 2007; plays an impo etention of gas (Jarvie, 2012). in-situ gas gene e of organic ma arma et al., 2 stin, 2007). Th hickness and ex d pressure, fluid 16, 2015a; Mis hale gas can e The shale gas f sins some of th Gondwana, Kri shale beds of b Das, 2013). Es IS ian Shale Beds g/10.1007/s1258 an Shal s Reser Damodhar K ka Bannerjee ndia anbad 826 004, a ad 826 004, Ind ince prelimina d to shale gas In this study, B aracteristics. It quartz and mi planes, signifyi s from 1.21 wt. nite and mine % to 9.05 vol. position substa e region. The l methane stora for pore blocki Type II sorpti structure main ore volume. eochemical (the variable depth e the unconven e and reservoir house of continu ; Schmoker, 19 ortant role in u that is ultimat Organic matt eration which i atter (Loucks et 014; Ross and he quality of s xtent, organic c d saturations an hra et al., 2016 emerge as an formations are hem are Jharia, shna-Godavari both Gondwan stimates of shale SSN 1674-487X of Jharia Basin 83-017-0779-8. e Beds rvoir Kamble 2 , e 1 India dia ary re- Ba- t is ca, ing .% ral %, an- ow age ing ion nly ermogenic gas) (Passey et al., ntional gas sys- r rocks for gas uous petroleum 995). The proc- unconventional tely cracked to er in shale re- is stored in the t al., 2009) and d Marc, 2009; hale reservoirs ontent, thermal nd permeability 6; Ruppel et al., important new spread over in , Raniganj, Bo- and Cauvery na and Tertiary e gas resources X n . ) , - s m - l o - e d ; s l y , w n - y y