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Hydrocarbon Vision 2030 (ஹைட்ரோகார்பன் தொலைநோக்கு ஆவணம் 2030)

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The survey area mainly comprises of three blocks, namely, Block-1, 2 and 3. The area includes the<br />

acreages held by ONGC as well as adjoining open acreages. The details about the blocks are as<br />

follows:<br />

Block<br />

Name of the area<br />

Approx. LKM<br />

1 Sector-VC:<br />

Banaskandi ML, Cachar Dist. PML and AA-94/1 (Assam,<br />

Manipur & Mizoram)<br />

7351LKM<br />

Grid: 500m x 5000m<br />

2 AA-ONN-2001/2 (Assam, Mizoram) 4722 LKM<br />

Grid: 500m x 5000m<br />

3 ML areas- Namti, Geleki, Geleki-Extn, SE-Geleki, and SE-<br />

Geleki Extension (Assam, Nagaland)<br />

322 LKM<br />

Grid: 500m x 2500m<br />

Total LKM 12395<br />

The above areas are largely mountainous, typical elevations from mountain top to valley ranges from<br />

50 to 1,000m, rugged terrain with jungle cover and sparse population.<br />

AEM-PTP passive source electromagnetic method<br />

Electromagnetic methods provide cheaper means of supplementing seismic data. These methods<br />

respond to resistivity contrast of the formations unlike seismic, which respond to acoustic impedance<br />

contrast. FTB regimes often have thin high velocity near surface layers, which acts as an acoustic<br />

barrier whereas EM methods yield better results. "Audio electro magnetic passive transient impulse<br />

(AEM-PTP)” is a passive source transient electromagnetic prospecting technique based on detection<br />

of transients of secondary electromagnetic field associated with upward fluid flow associated with<br />

REDOX activity. It is a proprietary technology of Pinemont, a subsidiary of McPhar International Ltd.<br />

In June 2015, representatives from Mcphar international presented the Pinemont AEM-PTP survey<br />

techniques at ONGC, Jorhat. Following positive feedback and subsequent discussions, McPhar has<br />

given a proposal to undertake a test survey over a small block, covering approximately 100 sq km.<br />

Passive seismic tomography<br />

Passive seismic tomography involves listening to the earth passively over time and using it to derive<br />

subsurface information. P and S-wave travel times help in understanding structural configuration of<br />

the subsurface and Vp/Vs provides lithological information. Passive seismic tomography has already<br />

been deployed in Sector VC and survey completed in November, 2011 and data delivered as per the<br />

deliverables by M/S Land Tech Enterprises. The survey resulted in:<br />

1. Vp/Vs values that helped in demarcating sand prone areas<br />

2. PST velocity field, which were used in reprocessing of a few 2D lines and 3D volume in the area to<br />

see any possible improvement.<br />

5.1.4.2 Enhancing exploration activities<br />

(i)<br />

Conversion of 2P to 1P reserves<br />

The term 2P is used to denote the sum of proved and probable reserves and 1P is frequently<br />

used to denote proved reserves. The best estimate of recovery from committed projects is<br />

generally considered to be the 2P (sum of proved and probable reserves). However, probable<br />

reserves are lower categories of reserves, commonly combined and referred to as “unproved<br />

reserves,” with decreasing levels of technical certainty. Probable reserves are volumes that are<br />

defined as “less likely to be recovered as proved, but more certain to be recovered than possible<br />

reserves”.<br />

67

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