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Zeitschriftenartikel zum Thema „MIKIR HILLS“

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Veröffentlicht am 18. Mai 2024

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1

Kayal, J. R., und Reena De. „Microseismicity and tectonics in northeast India“. Bulletin of the Seismological Society of America 81, Nr. 1 (01.02.1991): 131–38. http://dx.doi.org/10.1785/bssa0810010131.

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Abstract Three microearthquake surveys were carried out in Shillong Plateau, Mikir Hills, and Assam valley areas during 1984 to 1986. Some 422 events are relocated by the Homogeneous Station Method. The microseismicity map reveals intense crustal (10 to 40 km) activity beneath the Tura area of Shillong Plateau. The areas to the west of Shillong and the area around Mikir Hills also show high activity. The microseismicity map further shows major tectonic lineaments that are compatible with the Landsat Imagery lineaments and the major faults. Composite focal mechanisms of the microearthquakes show spatial variation of the tectonic stresses in the region. An ENE-WSW horizontal compressive stress is dominant in the Tura area, whereas a SE-NW horizontal compressive stress is dominant in the Shillong and Mikir Hills areas.

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2

Bera, S. K. „Modern pollen deposition in Mikir hills, Assam“. Journal of Palaeosciences 49, Nr. (1-3) (31.12.2000): 325–28. http://dx.doi.org/10.54991/jop.2000.152.

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In the present investigation eight surface samples collected in a transact from within the forest to open land around Diphu-Lumding areas or Karbi Anglong District (Lat. 25°2' & 26° 1' N: Long. 92°44' & 93°42' E) in Assam were studied with a view to construct pollen spectra from Mikir hills of Assam.

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3

Sera, S. K. „Early Holocene pollen data from Mikir Hills, Assam, India“. Journal of Palaeosciences 52, Nr. (1-3) (31.12.2003): 121–26. http://dx.doi.org/10.54991/jop.2003.1760.

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The pollen analytical studies of a 1.5 m deep soil profile (12210±110 years BP at 80 cm level) from Kaki Forest Division in Mikir Hills of Assam have been carried out. The pollen investigation of surface samples was made to understand the pollen/vegetation relationship in the forest. However, the study of surface samples does not fully cohere with the present day set up of vegetation. Palynological studies of the sediment profile indicate that since the last 15,000 years there have been three stages of vegetational developments followed by a reducing environment at the beginning (150-120 cm) reflecting directly on brief phases of climate such as arid, semi-arid and warm and humid. The abundance of grasses both cultivated as well as wild throughout the pollen diagram has revealed the existence of an open savanna forest for a long period. The arboreal vegetation is represented by mixed tropical and subtropical trees and shrubs. Both monolete and trilete ferns are well documented in the assemblage. Occurrence of some degraded pollen and spores indicate the biodegradation of microbiota as evidenced by the presence of fungal spores and hyphae in almost all the sediments. The low occurrence of extra regional plant taxa like Pinus, Picea, Abies, Larix, Betula and Alnus in the sediments is indicative of long distance transportation of pollen from high elevation.

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Prakash, U., und P. P. Tripathi. „Fossil woods of Leguminosae and Anacardiaceae from the Tertiary of Assam“. Journal of Palaeosciences 17, Nr. (1-3) (16.06.2022): 22–32. http://dx.doi.org/10.54991/jop.1968.535.

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Three fossil woods from the Tertiary of Assam are described here. One, resembling the modern wood of Lannea, is from a road cutting at mile-stone 9 on Dimapur-Diphu road in Mikir Hills, and the others comparable with Adenanthera and Swintonia are from near the town of Hailakandi (24°26'N; 92°32'E) in district Cachar. Recently, these have been briefly described by us (Prakash & Tripathi, 1967, 1968).

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5

Acharjee, Shukla, Shubhendu Shekhar, D. Majumdar, Neelratan Singh, Y. K. Mawale, Akhilesh Singh und B. K. Iyengar. „The Satellite Derived Digital Elevation Models of Mikir Hills, Karbi Anglong, Assam, India“. Journal of Scientific Research 65, Nr. 03 (2021): 31–35. http://dx.doi.org/10.37398/jsr.2021.650305.

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6

Dhurandhar, A. P., U. K. Pandey und Ch Raminaidu. „Petrochemistry and Sr, Nd, Pb Isotopic Characteristics of Basic Dykes of Mikir Hills, Assam“. Journal of the Geological Society of India 94, Nr. 6 (Dezember 2019): 559–72. http://dx.doi.org/10.1007/s12594-019-1361-z.

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7

Ghosh, Gopal K. „Automatic thrust/fault and edge location with gravity data across the Shillong plateau and Mikir hill complex in northeastern India using the most positive and most negative curvature interpretation“. Journal of Geophysics and Engineering 21, Nr. 1 (02.01.2024): 290–303. http://dx.doi.org/10.1093/jge/gxad101.

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Abstract Northeast India encompasses numerous thrusts, faults, and lineaments with undulated surface topography and is one of the utmost tectonically active regions in the world. Owing to the results of the collision of the Indian Plate under the Tibetan Plate and Burmese Plate, respectively, this area has affected the highest seismic potential zone-V, triggering many earthquakes. The current study area is located in and around the Shillong plateau, Mikir Hills, Naga Hills, Arakan-Yoma fold belt, Bengal basin, and Mishmi hills of the Himalayan foothills and that fall under the northeast of India. The thrusts and faults information available in this area are very scanty due to limited availability of geoscientific data and revealing seismic survey. Henceforth, it is necessary to get enhanced geoscientific learning for a better understanding of thrusts, faults, and lineaments information, the most positive and most negative curvature attribute analyses have been carried out using ground gravity data in this area. The significant derived results from this study encourage supplementary findings of thrust, fault, and lineament information, which also correlate well with the previously found results of 3D Euler deconvolution and source edge detection. Although, gravity data interpretation has its own limitations, however, the current derived results using the latest curvature analysis approach utilizing gravity data show realistic invigorated solutions for a better understanding of the thrust, fault, and lineament locations in this area.

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8

Tripathi, S. K. M., R. K. Saxena und Vandana Prasad. „Palynological investigation of the tura formation (early eocene) exposed along the tura-dalu road, west Garo Hills, Meghalaya, India“. Journal of Palaeosciences 49, Nr. (1-3) (31.12.2000): 239–52. http://dx.doi.org/10.54991/jop.2000.145.

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The present paper deals with the palynological study of the Tura Formation exposed along the Tura Dalu Road in West Garo Hills, Meghalaya. The recovered palynoflora is represented by dinoflagellate cysts, fungal remains, pteridophytic spores and angiosperm pollen. The assemblage is dominated by angiosperm pollen assignable to the families Arecaceae, Liliaceae, Oleaceae, Bombacaceae, Caesalpiniaceae, Mimosaceae, Unieaceae and Alangiaceae. Three new species of angiosperm pollen viz.. Retitricolpites singhii, Lanagiopollis meghalayaensis and Lanagiopollis subglobosus have been proposed. Pteridophytic spores, which constitute the subdominant clement of the assemblage, are assignable to the families Osmundaceae, Matoniaceae. Polypodiaceae. Sehizaeaceae and Parkeriaceae. Based on the quantitative analysis of the palynoflora, the studied sequence has been divided into three formal palynological assemblage zones. In ascending order, these are: (1) Lanagiopollis spp. Assemblage-zone (2) Palmidites spp. Assemblage-zone and (3) Tricolporopilites spp. Assemblage-zone. A comparison of the present assemblage with other Palaeogene assemblages of India indicates that it correlates well with those known from the upper pan of the Mikir Formation. Nonh Cachar Hills. Assam; the Prang Formation, Jaintia Hills Meghalaya; the Naredi Formation, Kutch; and the Rajpardi Lignite, Gujarat. Since these formations are of Early Eocene age, the studied sequence is also dated as Early Eocene. Most families represented in the assemblage are presently distributed in tropical to subtropical regions. indicating a similar climate during the deposition of Tura sediments. The presence of coastal elements and dinoflagellate cysts in the assemblage is indicative of a littoral depositional environment.

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9

Baruah, Saurabh, Dipok K. Bora und Rajib Biswas. „Estimation of crustal discontinuities from reflected seismic waves recorded at Shillong and Mikir Hills Plateau, Northeast India“. International Journal of Earth Sciences 100, Nr. 6 (21.05.2010): 1283–92. http://dx.doi.org/10.1007/s00531-010-0541-2.

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10

Biswal, Shantajhara, Kapesa Lokho, Annie Needham, Ansuya Bhandari, Uma Kant Shukla, Kezhakielie Whiso und Kuldeep Prakash. „Record of Additional Middle Eocene Vertebrate Remains from the Mikir Hills, NE India: Implications on Paleoenvironment and Paleobiogeography“. International Journal of Geosciences 13, Nr. 08 (2022): 609–26. http://dx.doi.org/10.4236/ijg.2022.138033.

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11

Saha, Abhishek, Sohini Ganguly, Jyotisankar Ray und Nilanjan Chaterjee. „Evaluation of phase chemistry and petrochemical aspects of Samchampi-Samteran differentiated alkaline complex of Mikir Hills, northeastern India“. Journal of Earth System Science 119, Nr. 5 (Oktober 2010): 675–99. http://dx.doi.org/10.1007/s12040-010-0052-3.

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12

Bora, Dipok K., und Saurabh Baruah. „Mapping the crustal thickness in Shillong–Mikir Hills Plateau and its adjoining region of northeastern India using Moho reflected waves“. Journal of Asian Earth Sciences 48 (April 2012): 83–92. http://dx.doi.org/10.1016/j.jseaes.2011.12.007.

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13

Sharma, Sangeeta, und Saurabh Baruah. „Modelling of the Kopili Fault based on slip rate, moment rate and seismic activity in Mikir Hills Plateau of Northeastern India“. Geomatics, Natural Hazards and Risk 8, Nr. 2 (28.04.2017): 1157–72. http://dx.doi.org/10.1080/19475705.2017.1300609.

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14

Rai, Neha, Dip Kumar Singha und Rima Chatterjee. „Assessment of Paleocene to lower Oligocene formations and basement to estimate the potential hydrocarbon reservoirs using seismic inversion: a case study in the Upper Assam Shelf, India“. Journal of Petroleum Exploration and Production Technology 12, Nr. 4 (18.11.2021): 1057–73. http://dx.doi.org/10.1007/s13202-021-01357-1.

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AbstractThe upper Assam shelf is a self-slope basin in north-east India, filled with nearly 7 km of sedimentary rocks of tertiary period with the granite basement and various oil fields along the border of the Naga thrust. The major producing fields are structural and strati-structural. The study area is placed in between the Mikir hills and Naga thrust. The objective of the study is to identify potential hydrocarbon reservoir zones in the geologically complex south upper of the Assam shelf using estimates of acoustic impedance and porosity derived by 3D post-stack seismic inversion. Well data, such as sonic velocity and density logs, from two wells (namely, KA and TE) are used in the inversion and validation of results. Inversion results are used to build a geological model in the form of acoustic impedance from which we derive 3D porosity cube which are used for hydrocarbon potential in the Paleocene to lower Oligocene sands, and the Precambrian basement. Although the amplitude maps provide an indication of potential reservoirs, the extent of these zones are much better identified in the inverted impedance maps and the corresponding estimated high-porosity zones. The analysis predicted the potential reservoir rocks in the Sylhet, Kopili and Barail formations, in which the Sylhet and Kopili appear to have good potential zones. Near the vicinity of the Naga thrust belt, the proximity of potential reservoir is predicted in the Kopili, Sylhet formation and in the fractured basement, respectively.

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15

Biswal, Shantajhara, Kapesa Lokho, Uma Kant Shukla, Kezhakielie Whiso und Kuldeep Prakash. „Eocene larger foraminiferal biostratigraphy, depositional history and paleogeography of the Sylhet Limestone of the Mikir Hills of Assam, NE India: Implications for an Open Tethys“. Micropaleontology 67, Nr. 5 (2021): 427–46. http://dx.doi.org/10.47894/mpal.67.5.01.

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This study presents results of integrated larger foraminiferal biostratigraphy, lithofacies and stable carbon isotope (13 C org) analysis carried out in the Sylhet Limestone of Dillai Parbat Limestone Mine succession, Karbi Anglong District, Assam. Larger foraminiferal assemblages assign a middle Eocene age to the studied succession of Sylhet Limestone. The Shallow Benthic Zone (SBZ) 13 and SBZ 16-18 and a barren interval in between is recognized in the studied part of the Sylhet Limestone. The SBZ 13 Zone (early Lutetian) is represented by fossiliferous limestone at the base of the section and is inferred to have been deposited in a subtidal environment. The overlying barren interval lies in the arenaceous interval and was likely deposited in a subtidal channel sand shoaling bars. The upper part of the section ismarked by SBZ16-18 (late Lutetian to Bartonian) and was deposited in subtidal channel sand inner neritic zone environments, followed by intertidal marl to subtidal limestone. The organic carbon stable isotopic data reveals a sharp negative excursion at about 34-35m of the succession, which may be correlated with Middle Eocene Climatic Optimum (MECO) and/or vegetation types. This and earlier studies from India and elsewhere indicate that during the middle Eocene, the Neo-Tethys Sea was open and connected through the East and West coasts of India, Northeast India, western Himalaya, and most of the Middle East and southeast Europe. This vast area produced enormous amount of petroleum.

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16

Saha, Abhishek, Sohini Ganguly, Jyotisankar Ray, Christian Koeberl, Martin Thöni, C. Sarbajna und S. S. Sawant. „Petrogenetic evolution of Cretaceous Samchampi-Samteran Alkaline Complex, Mikir Hills, Northeastern India: Implications on multiple melting events of heterogeneous plume and metasomatized sub-continental lithospheric mantle“. Gondwana Research 48 (August 2017): 237–56. http://dx.doi.org/10.1016/j.gr.2017.04.022.

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17

Mitra, N. D. „Indian Gondwana Plate margin and its evolutionary history“. Journal of Palaeosciences 36 (31.12.1987): 302–11. http://dx.doi.org/10.54991/jop.1987.1589.

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The outline of Indian Plate in the Gondwanaland Plate mosaic has been reconstructed. The basic premise for the reconstruction lies in the identification of the suture zone along Indus-Yarlung tectonic zone and Indo-Burman range, both of which are wreathed with ophiolite complexes. The north eastern margin of the Indian part of the Gondwana Plate, which was ill-defined in many earlier reconstructions, is now more precisely delineated with the find of slide-generated olistostrom bodies representing plate marginal trench setting around Ukhrul-Paoyi-Kiphire area of the ophiolite belt of Manipur-Nagaland. The recent report of continental Gondwanas close to this suture zone lends credence to this palaeogeographic reconstruction. On the north, the continental sediments having distinct Gondwana entity rarely extend to the Tethyan basin and as such the Indus-Yarlung Suture truly delimits the Gondwana Plate domain. The Himalayan front is regarded as Tethys-facing margin of the Gondwana continent. Along the eastern margin of Indian Plate, rifting as a sequel to ocean floor spreading led to the evolution of coastal troughs of Cauvery, Palar, Godavari-Krishna and Athgarh which bears records of marine transgressions during Aptian-Albian time from a juvenile Indian Ocean. These oceanward tilted troughs may represents the rifted arm of a triple junction formed during the continental fragmentation. The discovery of such troughs in the Upper Assam and Bengal Basin suggests that the separation of India from Eastern Gondwanaland occurred in a NE-SW direction. The Cambay and the Kutch basins document similar evolutionary history along the western margin of the Indian Plate. As a consequence of crustal tension accompanying the fragmentation, the outpour of tholeiitic basalt took place in Rajmahal, Khasi-Garo-Mikir Hills and Upper Assam at 100-105 million years along the west coast. The earliest manifestation of volcanism has been recorded in Saurashtra which is considered to be contemporaneous with Rajmahal volcanicity. It is suggested that both the eastern and western margins of the Indian Gondwana Plate bear closely related records of fragmentation in the Early Cretaceous time.

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Kumar, Santosh, Vikoleno Rino, Yasutaka Hayasaka, Kosuke Kimura, Shunmugam Raju, Kentaro Terada und Manjari Pathak. „Contribution of Columbia and Gondwana Supercontinent assembly- and growth-related magmatism in the evolution of the Meghalaya Plateau and the Mikir Hills, Northeast India: Constraints from U-Pb SHRIMP zircon geochronology and geochemistry“. Lithos 277 (April 2017): 356–75. http://dx.doi.org/10.1016/j.lithos.2016.10.020.

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19

Sarma, J. N., und S. Acharjee. „A GIS based study on bank erosion by the river Brahmaputra around Kaziranga National Park, Assam, India“. Earth System Dynamics Discussions 3, Nr. 2 (19.09.2012): 1085–106. http://dx.doi.org/10.5194/esdd-3-1085-2012.

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Abstract. The Kaziranga National Park is a forest-edged riverine grassland inhabited by the world's largest population of one-horned rhinoceroses, as well as a wide diversity of animals. The park is situated on the southern bank of the Brahmaputra River at the foot of the Mikir Hills. National Highway 37 forms the southern boundary and the northern boundary is the river Brahmaputra and covers an area of about 430 km2. The Brahmaputra River flows by Kaziranga National Park in a braided course for about 53 km. Sequential changes in the position of banklines of the river due to consistent bank erosion have been studied from Survey of India topographic maps of 1912–1916 and 1972, satellite IRS LISS III images from 1998 to 2008 using GIS. Study of bank line shift due to the bank erosion around Kaziranga has been carried out for the periods 1912–1916 to 1972, 1972 to 1998 and 1998 to 2008. The amounts of the bank area lost due to erosion and gained due to sediment deposition are estimated separately. The total area eroded during 1912–1916 to 1972 was more (84.87 km2) as compared to accretion due to sediment deposition (24.49 km2), the total area eroded was also more in 1972–1998 (44.769 km2) as compared to accretion (29.47 km2) and the total area eroded was again more in 1998–2008 (20.41 km2) as compared to accretion (7.89 km2). The rates of erosion during 1912–1916 to 1970, 1970 to 1998, and 1998 to 2008 were 1.46, 1.59 and 1.021 km2 per year, respectively. During the entire period (1912–1916 to 2008) of study the erosion on the whole was 150.04 km2 and overall accretion was 61.86 km2 resulting in a loss of 88.188 km2 area of the park. The maximum amounts of shift of the bankline during 1912–1916 to 1970, 1970 to 1998, and 1998 to 2008 were 4.58 km, 3.36 km, and 1.92 km, respectively, which amount to the rates of shift as 0.078, 0.12 and 0.096 km per year, respectively. A lineament and a few faults have controlled the trend of the course of the Brahmaputra around Kaziranga area. The main cause of erosion of the Brahmaputra is the loose non-cohesive sediments of the bank throughout the park. The braided channel of the river strikes the bank directly and undermines the silty bank causing overhanging blocks to be carried away easily by the river current. In future deposition is likely to be more in upstream or eastern part of Kaziranga and erosion in middle part of Kaziranga national park area due to the river Brahmaputra. Antierosion measures have been adopted only in a few places to check bank erosion at Kaziranga.

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Hussain, Bellal. „Sixth Schedule in Assam: An Overview“. RESEARCH REVIEW International Journal of Multidisciplinary 8, Nr. 12 (14.12.2023): 144–48. http://dx.doi.org/10.31305/rrijm.2023.v08.n12.021.

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Sixth schedule of Indian constitution is an integral part of Indian polity and a very important topic in current political domain. Assam is one of the tribal-dominated hill areas in the northeastern region, and this constitution is the only one of its kind to protect the cultural identities, habits, economic and political interests of the people who live there. The sixth schedule of the Indian Constitution lists four different councils: the regional council, the district council, the independent council, and the territorial council. That being said, Assam has three councils: two independent councils, one local council, and the state government. The North Cachar Hill area Council and the Mikir Hill District Council were both created after 1951. They are both in the Cachar area. It is mentioning here that the provision of six schedule has been reviewed time to time as per demand of different indigenous groups for autonomy. The sixth schedule of Indian constitution have both positive and negative affects. In this Article, it is tried to focus on some major problems as well as grievances of the deprived peoples of these living in the sixth schedule areas in Assam. Suggestions have also been provided to redress those problems and grievances.

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21

Krčmar, Stjepan, und Mislav Kovačić. „Diversity of horsefly fauna (Diptera: Tabanidae) of Bansko Hill“. Natura Croatica 32, Nr. 2 (30.12.2023): 523–34. http://dx.doi.org/10.20302/nc.2023.32.34.

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From 2018 to 2022, at 10 localities on Bansko Hill, 3,639 horseflies were sampled. Most specimens (3,404) were sampled in 2022 in the period from mid-May to mid-September. The horseflies sampled are classified into two subfamilies, six genera and 19 species. The species Hybomitra ukrainica (Olsufjev, 1952), Tabanus miki Brauer in Brauer and Bergenstamm, 1880, Haematopota grandis Meigen, 1820 and Haematopota pandazisi (Kröber, 1936) are new finds of horsefly species for the studied area. The species Tabanus tergestinus Egger, 1859 is the most abundant species and makes up 71.11% of the horseflies sampled. The species Tabanus bromius L., 1758 followed with 10.16% of the abundance, Tabanus sudeticus Zeller, 1842 with 8.82% and Atylotus loewianus (Villeneuve, 1920) with 5.74% of the horseflies sampled, while 15 other species of horseflies were represented by the remaining 4.17%. In the collected sample, male horseflies accounted for 51.71% of the sample; all of them were sampled with an oil liquid trap. The largest number of horseflies (84.14%) were sampled in localities on the northeastern side of Bansko Hill, covered with forest vegetation of secondary origin. Three species, T. bromius, T. tergestinus and Heptatoma pellucens, (Fabricius, 1776) have the longest flight period, from mid-May to mid-September. The highest peaks of abundance for T. tergestinus, T. bromius, and T. sudeticus were recorded in July, for H. pellucens in June and for A. loewianus in August. The greatest similarity in horsefly fauna (85.71%) was recorded in the localities Popovac and Karanac. 90.98% of horseflies were collected by liquid oil traps, followed by sticky traps (5.22%) and canopy traps (3.79%). Data from earlier studies from 2011 and data from the current studies in the area of Bansko Hill have yielded records of 22 species of horsefly.

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Jopang, Jopang. „KEBIJAKAN PEMBINAAN ATLET PUSAT PENDIDIKAN DAN LATIHAN PELAJAR DINAS KEPEMUDAAN DAN OLAH RAGA PROPINSI SULAWESI TENGGARA“. Journal Publicuho 1, Nr. 1 (10.04.2018): 1. http://dx.doi.org/10.35817/jpu.v1i1.5846.

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Kamra, Charu, Sumer Chopra und R. B. S. Yadav. „Tectonic stress of northeastern Indian region derived from seismic focal mechanisms and the effect of focal mechanism on stress drop: A comparative analysis with Kachchh intraplate region of India“. Geophysical Journal International, 22.02.2023. http://dx.doi.org/10.1093/gji/ggad083.

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Summary In this study, the focal mechanism solutions and source parameters of recent earthquakes that occurred in the northeastern region of India have been determined. The region has very complex tectonics as it is subjected to the compressional forces from all sides, due to the collision of the Indian Plate with the Eurasian, Burma, and Tibetan plates. Waveform data from deployed broadband seismographs (BBS) and strong motion accelerographs (SMA) in the northeastern India are used to determine the focal mechanism solutions and source parameters of moderate earthquakes respectively. The estimated focal mechanisms are used to understand the existing stress field in the region. It is found that the Shillong-Plateau as well as the Indo-Burma subduction zone is dominated by the compressional tectonic regime, Mikir-Hills and Bengal basin are dominated by the trans-tension tectonic regime, and the easternmost Himalayan region is dominated by the strike-slip tectonic regime. The maximum horizontal stress direction Shmax is also determined for above sub-regions. The direction of Shmax is southeast in the Bengal basin, northeast in Mikir-Hills, and Indo-Burma subduction zone whereas it is NNE in Shillong Plateau and SSW in the eastern Himalayas. The estimated stress drop value of the earthquakes in the region ranges from 2.11 to 23.89 MPa. The relationship between the source parameters and focal mechanisms is also explored. It is found that the earthquakes with a strike-slip mechanism have the highest average stress drop (7.05 MPa) followed by reverse (6.82 MPa) and normal (5.12 MPa) in the northeastern region of India. According to the examined data set, the stress drop is found to be dependent on the type of focal mechanism, seismic moment, and hypocentral depths. The comparison of the results with the Kachchh intraplate region in western India shows earthquakes in Kachchh have larger mean stress drop for all types of mechanisms. In both intraplate and interplate regions of India, the stress drop of earthquakes depends on the type of focal mechanism solution.

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Srivastava, Rajesh K., Vincenza Guarino und Leone Melluso. „Early Cretaceous ultramafic-alkaline-carbonatite magmatism in the Shillong Plateau-Mikir Hills, northeastern India – a synthesis“. Mineralogy and Petrology, 05.04.2022. http://dx.doi.org/10.1007/s00710-022-00777-z.

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AbstractA comprehensive mineralogical, geochemical and isotopic review of six ultramafic-alkaline-carbonatite magmatic intrusions of the Shillong Plateau (Sung Valley, Jasra, Swangkre-Rongjeng, and Mawpyut) and Mikir Hills (Samchampi-Samteran and Barpung) is presented here, using the published data. These intrusions emplaced ca. 115–102 Ma ago, thus are significantly younger than the tholeiitic flood basalts erupted in Rajmahal-Sylhet province (ca. 118–115 Ma). The intrusive lithologies vary from ultramafic (dunites, clinopyroxenites, melilitolites) to mafic (ijolites, gabbros sensu lato, shonkinites), to felsic (syenites, nepheline syenites) and carbonatites (mostly calcite-rich varieties). The volcanic-subvolcanic facies (lamprophyres, phonolites) are not abundant. The range of chemical compositions of the magmatic phases in the various assemblages is notable; the intrusive rocks are thus the result of crystallization of magmas from variably evolved, independent liquid-lines-of descent, generally of alkaline/strongly alkaline lineages and sodic-to-potassic in affinity. The large variations of the Sr–Nd isotopic ratios of the silicate intrusive rocks (sensu lato) suggest a role of shallow-level crustal contamination during their formation. The carbonatites of the Sung Valley and Samchampi-Samteran have different isotope ratios than the associated silicate rocks, have some isotopic affinity with the Group I tholeiitic basalts of Rajmahal Traps and have an ultimate genesis in a carbonate-bearing lithospheric mantle.

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Lokho, Kapesa, JosÉ Francisco Carrasco, Shantajhara Biswal, Kezhakielie Whiso und Ansuya Bhandari. „First report of Eocene echinoids from the Sylhet Limestone, Mikir Hills of Assam, India: palaeontological, palaeogeography and palaeoenvironmental significance“. Journal of the Palaeontological Society of India, 05.11.2023. http://dx.doi.org/10.1177/05529360231205313.

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This article reports two echinoid taxa viz. Ilarionia sindensis Duncan and Sladen (1884) and Porocidaris schmidelii Münster in Goldfus (1830) from the middle Eocene Sylhet Limestone of Mikir Hills, Assam. P. schmidelii is found from the Lutetian (middle Eocene) to the Priabonian (upper Eocene) in the following regions: NE of Spain, Biarritz (Southwestern France), Angoumé (Southern Aquitaine, France), Carinthia (Southern Austria), Venetian region of Italy Provence, Southern Alps of French, Istria (Croatia), Persian Gulf, Oman and Egypt. I. sindensis was first reported from the Eocene of Sindh province from the Khirthar Series (Pakistan) and Madagascar. It is also recorded from the Bartonian–Priabonian in the following regions: NE Spain, Biarritz in Southwestern France, Angoumé in Southern Aquitaine-France, Carinthia in Southern Austria, Italian region of Veneto, Provence and southern French Alps, Persian Gulf, Oman, Egypt and Istria. They are systematically described to know their stratigraphic, palaeoenvironment and palaeogeographic distribution. The material studied herein represents the first report from the middle Eocene of India, and it significantly expands the geographical extension of Eocene marine echinoids in the northeastern part of India.

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Hussain, M. Faruque, und Talat Ahmad. „Geochemical characteristics of the Granitoids of Mikir Hills Massif of Shillong Plateau, Northeast India: Implication for Pan-African Magmatic Activity“. Journal of the Virtual Explorer 32 (2009). http://dx.doi.org/10.3809/jvirtex.2009.00250.

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Nag, Rahul, H. Hrushikesh, Nathan Cogné und N. Prabhakar. „Late Neoproterozoic to early Cambrian high-grade metamorphism from Mikir Hills (Assam-Meghalaya gneissic Complex, northeast India): Implications for eastern Gondwana assembly“. Geoscience Frontiers, Mai 2024, 101850. http://dx.doi.org/10.1016/j.gsf.2024.101850.

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Sharma, Sangeeta, Jogendra Sarma und Saurabh Baruah. „Dynamics of Mikir hills plateau and its vicinity: Inferences on Kopili and Bomdila Faults in Northeastern India through seismotectonics, gravity and magnetic anomalies“. Annals of Geophysics 61, Nr. 3 (02.08.2018). http://dx.doi.org/10.4401/ag-7516.

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Kumar, Amit, Naresh Kumar, Sagarika Mukhopadhyay und Simon L. Klemperer. „Tomographic Image of Shear Wave Structure of NE India Based on Analysis of Rayleigh Wave Data“. Frontiers in Earth Science 9 (08.10.2021). http://dx.doi.org/10.3389/feart.2021.680361.

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The major scientific purpose of this work is to evaluate the geodynamic processes involved in the development of tectonic features of NE India and its surroundings. In this work, we have obtained tomographic images of the crust and uppermost mantle using inversion of Rayleigh waveform data to augment information about the subsurface gleaned by previous works. The images obtained reveal a very complicated tectonic regime. The Bengal Basin comprises a thick layer of sediments with the thickness increasing from west to east and a sudden steepening of the basement on the eastern side of the Eocene Hinge zone. The nature of the crust below the Bengal Basin varies from oceanic in the south to continental in the north. Indo-Gangetic and Brahmaputra River Valleys comprise ∼5–6-km-thick sediments. Crustal thickness in the higher Himalayas and southern Tibet is ∼70 km but varies between ∼30 and ∼40 km in the remaining part. Several patches of low-velocity medium present in the mid-to-lower crust of southern Tibet along and across the major rifts indicate the presence of either partially molten materials or aqueous fluid. Moho depth decreases drastically from west to east across the Yadong-Gulu rift indicating the complex effect of underthrusting of the Indian plate below the Eurasian plate. Crust and upper mantle below the Shillong Massif and Mikir Hills are at a shallow level. This observation indicates that tectonic forces contribute to the uprising of the Massif.

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Firoze Dotiwala1, Sucheta Dotiwala1. „Abstract: A Study Of The Lineament Fabric Of The Mikir Hills Using Satellite Remote Sensing Data On A GIS System For Inputs To Exploration In The Dhansiri Valley, Assam, India“. AAPG Bulletin 84 (2000) (2000). http://dx.doi.org/10.1306/c9ebd58f-1735-11d7-8645000102c1865d.

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Choudhuri, Mainak, Prabir Routray, Bikashkali Jana und Sudhir Mathur. „Timing the Mikir Hill uplift in Assam Basin: Record of stress propagation along the eastern margin of the Indian Plate“. Journal of Asian Earth Sciences: X, Januar 2023, 100137. http://dx.doi.org/10.1016/j.jaesx.2023.100137.

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