Tectonics of bengal basin or Bangladesh

Tectonics of bengal basin or Bangladesh

• 1.
  TECTONICS OF BENGALBASIN Overview TECTONIC SET UP OF BENGAL BASIN  TECTONIC MAP OF BENGAL BASIN  DEVELOPMENT OF BENGAL BASIN  TECTONIC ELEMENTS OF BENGAL BASIN
• 2.
  The first tectonicmap of the then East Pakistan was prepared in 1964. Concise characteristics of basic tectonic elements of the then East Pakistan and its neighbouring areas were prepared in 1965 while the major tectonic features of the then East Pakistan were compiled in 1966. Tectonic map of Assam was published in 1964 and the tectonic classification of Bangladesh was made in 1972. On the other hand tectonic framework and oil and gas prospects of Bangladesh were published in 1978. The tectonic map of Bangladesh- past and present was introduced in 1983. It is essential to have a clear conception about the tectonic framework of Bengal Basin/Bangladesh in order to evaluate the prospect of MINERAL RESOURCES including oil and NATURAL GAS. TECTONICS OF BENGAL BASIN/Bangladesh
• 3.
  The Bengal basinoccupies most of Bangladesh and West Bengal subsurface. The extent of the basin is indirectly indicated by the hills surrounding it. To the south the basin is open to the Bay of Bengal, where it passes to the Bengal deep-sea Fan. It slopes south from its head at latitude 200 north to 100 south. The Bengal deep-sea fan is almost 3000km long and 1000km wide with a thickness of more than 12 km of sediments. Sediments from delta are funneled south through the “Swatch of No Ground” (submrine canyon), to become spread out on the fan by turbidity currents. Shield areas are exposed on sides of the Bengal basin with dis- appearance below a blanket of alluvium within the basin. The Precambrian shields are mainly constituted of gneisses and meta- sediments and local granites. The Shillong Plateau and the Precambrian shield of Bihar and West Bengal are separated from each other by the Garo-Rajmahal Gap which is 200km wide and controls the big bends of Ganges and Brahmaputra rivers. The Rajmahal and Garo hilla are connected by a submerged basement ridge (Rangpur saddle) at a depth of 200m.
• 4.
  Map showing majortectonic elements in and around the Bengal basin. Hinge zone demarcates the deeper basin from the Indian Platform area. Right-lateral N–S faults (e.g., Kaladan fault) are in the east. The Dauki fault separates the Sylhet trough from the uplifted Shillong Plateau at the north
• 5.
  Bangladesh is dividedinto two major tectonic units: i) Stable Pre-Cambrian Platform/Shelf in the northwest, and ii) Geosynclinal basin in the southeast. iii) A third unit, a narrow northeast-southwest trending zone called the hinge zone separates the above two units almost through the middle of the country. This hinge zone is currently known as palaeo-continental slope.
• 6.
  Stable Pre-Cambrian Platform: Stable Pre-Cambrian Platform also refers to as the stable shelf of the BENGAL BASIN. It is the part of the basin that lies on the west and northwest of the line joining Calcutta and MYMENSINGH known as Calcutta- Mymensingh gravity high, which represents the hinge zone of the basin or the basin ward extension of the stable shelf. The stable shelf is divided into three major zones : i) Dinajpur slope, ii) Rangpur Saddle and iii) Bogra slope. The stable shelf is composed of continental crust overlain by Cretaceous (144 to 66 million years ago) to Recent sediments. However, in isolated basins on the stable shelf, there is Permo-Carboniferous (360 million years to 245 million years ago) sediments with considerable amount of COAL. The thickness of sedimentary column on the stable shelf of Bengal Basin varies from less then 200m to 8,000m. A large part of the basin is covered by Sylhet limestone of Eocene age (58 million years to 37 million years ago) and act as a marker horizon to define the basin ward extent of the stable shelf. In Bangladesh part coal, LIMESTONE and HARDROCK are considered to be major mineral resources found on the shelf. However, there are evidences that precious metal and base metal of Indian shield may also be present. TECTONIC ELEMENTS
• 7.
  The tectonic frameworkof Bangladesh can be divided into two main elements: the Indian platform comprising the north western part and the Bengal foredeep representing the thick sedimentary column forming geosynclinal area in the south east. These two elements are separated by a flexure zone named as “Calcutta- Mymenshing hinge zone”. Further the Bengal foredeep is divided into two parts the folded flank in the east and platform flanks on the west which is demarcated by “Barisal high”. The platform flanks includes Sylhet trough, Faridpur trough, Hatiya trough and the Madhupur high structures. The deepest part of Bengal Basin is the Patuakhali trough (Figure 7).
• 8.
  Rangpur Saddle: It representsIndian Platform and connects the Indian Shield with the SHILLONG MASSIF and the Mikir Hills. Shillong Massif is a large thrust block of the Indian Shield. In Rangpur Saddle the basement is the most uplifted and is covered with thin sedimentary deposits. In Madhyapara area of DINAJPUR the basement is only 130m deep from the ground surface and is overlain by Dupi Tila Sandstone and Madhupur Clay of Plio-Pliestocene age. Rangpur Saddle can be divided into 3 parts- Rangpur Saddle, Northern Slope of Rangpur Saddle and Southern Slope of Rangpur Saddle. It is evident from seismic data acquired out by OGDC (Oil and Gas Development Corporation) during 63-64 in Rangpur-Dinajpur districts that both the northern and the southern slopes of Rangpur Saddle are quite gentle. The basement plunges gently from Madhyapara towards the southeast upto the Hinge Zone, which is known as the Southern Slope of Rangpur Saddle. The tentative boundary of the Rangpur Saddle with the northern and the southern slopes has been marked at approximately 700m contour line on the basement. It separates the Bengal Foredeep and the Himalayan Foredeep. TECTONIC ELEMENTS
• 9.
  Dinajpur Slope: TheNorthern Slope of Rangpur Saddle also known as Dinajpur Slope, occupies the north western part of Rangpur-Dinajpur districts and gently slopes towards the Sub-Himalayan Foredeep with dips 3-4° which sharply increases in Tetulia area. The only well drilled in 1988 located on the north-western most tip of Bangladesh at SALBANHAT by Shell for oil and gas exploration to probe a carbonate reef ended in basement with depth 2518m penetrating the Mio-Pliocene sequence without encountering Eocene Limestone. The nature of junction between the Dinajpur Slope and the Sub-Himalayan Foredeep is not clear. Bogra Slope/Shelf: represents the southern slope of Rangpur Saddle which is a regional monocline plunging towards southeast gently to Hinge Zone. This zone marks the transition between the Rangpur Saddle and the Bengal Foredeep from depositional as well as structural point of view. The width of Bogra Shelf varies from 60-125 km up to the Hinge Zone and the thickness of the sedimentary sequence increases towards the southeast. Stanvac Oil Company (SVOC) carried out aeromagnetic and seismic surveys in the mid-fifties followed by two wells at Kuchma and BOGRA. Seismic contours on top of Eocene Limestone (Bogra limestone) show regional dip of 2-3° besides revealing a number of NE-SW trending faults of which BOGRA FAULT is the most prominent. The attitude of Sylhet Limestone most possibly reflects the surface of the Archean Basement. There is no closed anticlinal fold in this tectonic zone. The Bogra fault did not provide the seal to the structural trends at Kuchma and Bogra for accumulation of commercial HYDROCARBONs. TECTONIC ELEMENTS
• 10.
  Calcutta-Mymensingh Gravity High:It reflects a tectonic element known as Hinge Zone and more recently as palaeo-continental slope in the framework of Bangladesh. The Hinge Zone is a narrow strip of about 25 km wide complex flexure zone, which separates the Bengal Foredeep from the shelf zone. It trends approximately N 30° E along the Calcutta-Pabna-Mymensingh gravity high and extends upto the western tip of Dauki fault. This zone is characterised by the sharp change in the dip of the basement rocks associated with deep-seated displacements in faults and is reflected on the gravity and magnetic anomalies. The Eocene limestone dips at about 200 in this zone as compared to 2-30 in the shelf zone. The seismic interpretation shows that the depth of the Sylhet Limestone - a strong seismic reflector - increases from 4000m to 9000m within a narrow zone of 25-km. Hinge Zone is connected with Bengal Foredeep by deep basement faults that probably started with the break up of Gondwanaland. Since then they have been repeatedly reactivated. In the northeast of Bangladesh the Hinge Zone turns to the east and seems to be connected with the Dauki Fault, probably by a series of east- west trending faults. TECTONIC ELEMENTS
• 11.
  Geosynclinal Basin thegeosynclinal basin in the southeast is characterised by the huge thickness (maximum of about 20 km near the basin centre) of clastic sedimentary rocks, mostly sandstone and shale of Tertiary age. It occupies the greater Dhaka-Faridpur- Noakhali-Sylhet-Comilla-Chittagong areas. The huge thickness of sediments in the basin is a result of tectonic mobility or instability of the areas causing rapid subsidence and sedimentation in a relatively short span of geologic time. The geosynclinal basin is subdivided into two parts i.e fold belt in the east and a foredeep to the west. Bengal Foredeep occupies the vast area between Hinge Line and Arakan Yoma Folded System and plays the most important role in the tectonic history of Bengal Basin. Tectonically, Bengal Foredeep can be divided into two major regions- (a) Western Platform Flank and (b) Eastern Folded Flank. The Western Platform flank is further subdivided into (a) Faridpur Trough (b) Barisal-Chandpur High (c) Hatiya Trough (d) Madhupur High and (e) Sylhet Trough. Faridpur Trough situated adjacent to Hinge Zone is characterised by a general gravity low with development of Neogene sequence. Sylhet Limestone is 6500 m deep in area south of the confluence of the PADMA and the JAMUNA. Chalna and BAGERHAT are the two notable structural highs of very low amplitude.
• 12.
  Hatiya Trough representsthe deepest trough of Bengal Basin, which received highest accumulation of clastic sediments. The axis of Bengal Foredeep runs through the apex of Hatiya Trough. Shahbazpur (BHOLA), Kutubdia, Sangu and a large number offshore structures are located here, of which Sangu is under production while Shahbazpur and Kutubdia are awaiting development. Madhupur High is represented by Pleistocene terrace of Madhupur Garh separates Faridpur Trough from the Sylhet Trough (SURMA BASIN). Here, the basement is relatively uplifted as evident from gravity and aeromagnetic data. Morphological studies reveal a pronounced recent morphological upheaval east of Madhupur. Besides, Nagarpur dome, south of TANGAIL and Nandina high showed that these are portions in the basement without deforming the sedimentary sequence overlying these features. Madhupur or Mymensingh High: the area represents an undulated TOPOGRAPHY slightly elevated from the adjacent active FLOODPLAIN. At MADHUPUR, tectonic disturbances can easily be observed where Dupi Tila sand is exposed under the Madhupur Formation. Most of the authors believe that the MADHUPUR TRACT represents a tectonically uplifted surface. A few also believe that the area was uplifted in very recent time and referred to the EARTHQUAKE of 1762 as the Madhupur tract occurs along the axis of the belt of 'Volcano action', extends in a north-western direction through CHITTAGONG and DHAKA. They considered numerous low lakes in the Sylhet basin to be caused by SUBSIDENCE compensatory to the elevation of the Madhupur tract. According to their belief, the uplift of Madhupur tract resulted the diversion of the BRAHMAPUTRA River.
• 13.
  Barisal-Chandpur High isinterpreted as a gravity and magnetic anomaly caused by a magmatic body at great depth. This zone is located between Faridpur trough and Hatiya trough of the Bengal Foredeep. The width of the zone is about 60 km and apparently corresponds to an uplift of the sedimentary cover. A number of gravity anomalies are spread over this zone. A paleo-high stretching from Barisal-Chandpur High in the NE direction has been presumed and the ridge was interpreted to turn south of Barisal-Chandpur High in north- south direction merging with the Ninety east ridge. There is no definite evidence for existence of such a ridge dividing the Bengal Foredeep into two parts. PATHARGHATA, MULADI, CHANDPUR, LAKSHMIPUR [Laksmipur], MUNSHIGANJ, Kamta and DAUDKANDI are the main anticlinal structures of this zone. Muladi wells failed to yield positive result in respect of commercial accumulation of HYDROCARBONs due to lack of northern closure. This zone has not been sufficiently investigated by seismic surveys.
• 14.
  Sylhet Trough: IndianPlatform bounds the trough from the west while it is open in the southwest to the main part of Bengal Basin. It is an oval shaped trough about 130 km long and 60 km wide. Sub-meridional trending anticlinal folds of Chittagong-Tripura Folded Belt gradually plunge northward to the Sylhet Trough. In cross-section the Sylhet Trough is sharply asymmetrical with comparatively gentle southern and steep faulted northern slope. Sylhet Trough is situated on the southern side of the Shillong Massif and corresponds to the vast low lands of Surma Valley with numerous swamps (haors) where absolute elevation marks even below the sea level. It is a sub- basin of the Bengal Foredeep in the northeastern part of Bangladesh and is characterised by a very pronounced, vast, closed negative gravity anomaly up to 84 mgl (Milligal). Shillong Massif forms the northern boundary of Sylhet Trough while the great Dauki Fault separates the trough from the Massif. The Trough is bounded on the east and southeast by the sub-meridional trending folded belt of Assam and Tripura as the frontal deformation zone of Indo- Burman Ranges.
• 15.
  Dauki Fault with5 km wide fault zone forms the contact between Shillong Massif and Sylhet Trough. The evolution of Sylhet Trough includes (i) a passive continental margin (Pre-Oligocene) to (ii) a foreland basin linked to the Indo- Burman Ranges (Oligocene and Miolene) to (iii) a foreland basin linked to south- directed over thrusting of Shillong Plateau (Pliocene-Holocene). The anticlinal folds of Habiganj, Rashidpur, Bibiana, Maulvi Bazar, Katalkandi, Fenchuganj, Harargaj, Patharia, Beani Bazar (Mama Bhagna) and Kailas Tila, which occupy the southern rim of Sylhet Trough have sub-meridional trend in contrast to sub- latitudinal trending Chhatak, Jalalabad, Sylhet, Dupi Tila and Jatinga structures. These two structural trends form a syntaxial pattern at the northeastern tip of Sylhet Trough. The Neogene sediments have excellent development in Sylhet Trough while the Paleogenes are at greater depths. Sylhet Trough is the most prospective petroliferous province of Bangladesh with 10 gas fields (Chhatak, Jalalabad, Sylhet, Kailas Tila, Beani Bazar, Fenchuganj, Rashidpur, Maulvi Bazar, Bibiana and Habiganj) of which Jalalabad, Sylhet, Kailas Tila, Rashidpur and Habiganj are producing now about 1000 million cubic feet per day (MMCFD) for generation of power, manufacture of FERTILISER besides meeting the industrial, commercial and domestic needs to a great extent thus contributing immensely to the economic development of Bangladesh.
• 16.
  Folded Belt representsthe most prominent tectonic element of Bengal Foredeep with general sub-meridional trending hills parallel to the Arakan Yoma Folded System. Folded belt extends within Bangladesh for 450 km (N-S) and about 150 km wide covering an area of 35,000 sq km of on-shore area. A large number of narrow, elongated N-S trending folds of the eastern part of Bangladesh (Sylhet and Chittagong Divisions), Tripura, southern part of Assam, Mizoram and Myanmar territory adjacent to S-E of the Chittagong Hill Tracts occupy the Folded Belt west of the Arakan Yoma Folded System. The folds are characterised by ridge forming, box-like in cross section, high amplitude with variable width and lie en-echelon with the adjacent structures. The elevation of these elongated anticlinal folds in Bangladesh ranges from 100 -1,000m. Some of the structures are faulted and thrusted and the intensity of folding increases gradually from west to east. Consequently, the structures of the eastern part are tightly folded, faulted and thrusted with narrower synclines between them.
• 17.
  The Folded Beltis sub-divided into two tectonic zones- Western Zone and Eastern Zone according to the intensity of folding and other structural features. Western Zone consists of relatively simpler GEOLOGICAL STRUCTURES like Beanibazar (Mama Bhagna), Kailas Tila, Fenchuganj, Kathalkandi, Maulvi Bazar, Rashidpur, Habiganj, Titas, Rokhia (Saldanadi), Lalmai, Trichna, Agartala, Lambusara, Gojalia, Feni, Semutang, Halda, Lambaghona, Maheshkhali, Patiya, Inani, St Martin besides the moderately tight folded anticlines like Bachia, Langtrai, Barmura, Atharamura, Dhumbura, Tulamura, Changotang, Sardeng, Gobamura, Sitapahar, Bandarban, Matamuhari, Olah Taung, Dakhin Nila etc and Mayu, Pingna and Sin in Myanmar. The Eastern Zone includes Patharia, Harargaj, Chargola, Kanchanpur, Machlithum, Sarkhan, Langai, Badarpur, Chatrachura, Masimpur, Rengte, Bhuban, Bhairabi, Hatch Hak, Sentet, Zanlawn, Zabwak, Maul Vawm, Jampai, Bhuachari, Shishak, Kasalang, Barkal, Utanchatra, Belasari, Gilasari, Mowdok, Langsen, Thuamphui, Maurawap, Phalphang and Kaletwa. (Dashed structures are in Bangladesh rest in Assam, Tripura and Mizoram of India). The Western Zone is the most important and prospective oil and gas province of Bangladesh with 12 fields from north to south eg Kailas Tila, Beanibazar, Fenchuganj, Maulvi Bazar, Rashidpur, Bibiana, Habiganj, Titas, Bakhrabad, Rokhia, Feni and Semutang. TECTONIC ELEMENTS Contd