The Cambay rift Basin, a rich Petroleum Province of India, is a narrow, .. Throughout the geological history, except during early syn– rift stage, the North. Petroleum Geology of the Cambay Basin, Gujarat., India. Front Cover. L. R. Chowdhary. Indian Petroleum Publishers, – Petroleum – pages. Petroleum geology of the Cambay Basin, Gujarat., India. Responsibility: L.R. Chowdhary. Imprint: Dehradun: Indian Petroleum Publishers, c Physical.

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The NW-SE Dharwarian tectonic trends got rejuvenated creating a narrow rift graben extending from the Arabian sea south of Hazira geoloyg beyond Tharad in the north.

This shale sequence has been divided into Older and Younger Cambay Shale with an unconformity in between. Throughout the geological history, except during early syn— rift stagethe North Cambay Basin received major clastic inputs from north and northeast, fed by the Proto—Sabarmati and Proto—Mahi rivers.

Cambay Basin

At places a gradational contact with the overlying Cambay Shale has also been noticed. Pliocene was a period of both low and high strands of the sea level, allowing the deposition of sand and shale. The discovery of oil in Ankleshwar structure in gave boost to the exploration in the Cambay Basin. The magnetic anomaly map also depicts the broad structural configuration of the basin. Cambay Basin Basin Introduction: From north to south, the blocks are:.

Subsequently, there was a strong tectonic activity that resulted in the development of the Mehsana Geollgy and other structural highs associated with basement faults. The same is true for the Tarapur Shale. Trap Rock The most significant factor that controlled the accumulation of hydrocarbons in the Olpad Formation is the favorable lithological change with structural support and short distance migration.

Similarly, the Proto—Narmada river system was active in the south, supplying sediments from provenance, lying to the east. Based on the cross trends the basin has been divided into five tectonic blocks. Reservoir Rock There are a number of the reservoirs within the cambayy sequence of the Olpad Formation.

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There was a regional southward tilt of the entire rift basin during Late Eocene and it is marked by a regional marine transgression extending far to the north upto Sanchor basin. The associated unconformity also helped in vambay development of secondary porosity. The Early Tertiary sediments ranging in age from Paleocene to Early Eocene represent syn-rift stage of deposition that was controlled by faults and basement highs in an expanding rift system.

Gradually, the rift valley expanded with time. The end of deposition of the Olpad Formation is marked by a prominent unconformity.

Petroleum geology of the Cambay Basin, Gujarat., India in SearchWorks catalog

During Miocene The depocenters continued to subside resulting in the deposition of enormous thickness of Miocene sediments as the Babaguru, Kand and Jhagadia formations. The end of Cambay Shale deposition is again marked by the development of a widespread unconformity that is present throughout the basin.

Different Tectonic Zones with in the Basin The Cambay rift valley is bounded by well demarcated basin margin step faults. The total volume of seismic reflection data acquired from the Cambay Basin is of the order of LKM 2D and sq. The Bouguer anomaly map has helped in identification of the major structural highs and lows in the basin.

These consist of sand size basalt fragments. The Middle Eocene witnessed a regressive phase with oscillating conditions of deposition and development of deltaic sequences in the entire basin.

During Paleocenethe basin continued to remain as a shallow depression, receiving deposition of fanglomerate, trap conglomerate, trapwacke and claystone facies, especially, at the basin margin under a fluvio—swampy regime.

The lithological heterogeneity gave rise to permeability barriers, which facilitated entrapment of hydrocarbons. The formation of the Cambay Basin began following the extensive outpour of Deccan basalts Deccan Trap during late Cretaceous covering large tracts of western and central India. A total of more than 30, LKM of conventional data has been acquired. The end of the Paleogene witnessed a major tectonic activity in the basin resulting in the development of a widespread unconformity.

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In the following period, relative subsidence of the basin continued leading to the accumulation of the Younger Cambay Shale.

In the geoloy part of the Ahmedabad-Mehsana Block, coal, which is well developed within the deltaic sequence in Kalol, Sobhasan and Mehsana fields, is also inferred to be an important hydrocarbon source rock.

Geographic Location of the basin The Cambay rift Basin, a rich Petroleum Province of India, is a narrow, elongated rift graben, extending from Surat in the south to Sanchor in the north.

Seismic and drilled well data indicate a thickness of about 8 km of Tertiary sediments resting over the Deccan volcanics. Shales within the Miocene section in the Broach depression might have also acted as source rocks.

This site is best viewed using current versions of Firefox v. Subsidence of the basin resulted in the accumulation of a thick sequence of euxinic black shales with subordinate coarser clastics.

During Early Eocenea conspicuous and widespread transgression resulted in the deposition of a thick, dark grey, fissile pyritiferous shale sequence, known as the Cambay Shale. Besides this, localized sandstone reservoirs within the Cambay Shale as in the Unawa, Linch, Mandhali, Mehsana, Sobhasan, fields, etc are also present. In the north, the basin narrows, but tectonically continues beyond Sanchor to pass into the Barmer Basin of Rajasthan.

cambaay

During Pleistocene to Recent, the sedimentation was mainly of fluvial type represented by characteristic deposits of coarse sands, gravel, clays and geopogy followed by finer sands and clays, comprising Gujarat Alluvium. The end of this sequence is marked by a regressive phase leading to deposition of claystone, sandstone, and shale alternations and a limestone unit of the Dadhar Formation.

Last modified: April 2, 2020