A review on deformation structures of different terranes in the Precambrian Aravalli-Delhi Mobile Belt (ADMB), NW India: Tectonic implications and global correlation

Biswal, Tapas Kumar; Pradhan, Rudra Mohan; Sharma, Neeraj Kumar; Tiwari, Shalbha; Beniest, Anouk; Behera, Bhuban Mohan; Singh, Suneet; Saraswati, Ragini; Bharadwaj, Anamika; Umasankar, B. H.; Singh, Yengkhom Kesorjit; Sarkar, Sounak; Mahadani, Tanushree; Saha, Gouri

doi:10.1016/j.earscirev.2022.104037

Cited by 10 publications

(12 citation statements)

References 101 publications

(186 reference statements)

Supporting

Mentioning

Contrasting

Order By: Relevance

“…According to Singh et al (2010) explanation, the granulites are thought to have exposed through the action of thrusting along a number of ductile Table 5. Comparison of geochemical values of the pelitic granulite of the study area with rocks of different tectonic settings (Bhatia, 1983;Bhatia, 1985;Bhatia & Crook, 1986 shear zones during the transition from syn-to post-F 2 folding (Bhowmik et al Singh et al 2010, 2020Tiwari & Biswal, 2019;Biswal et al 2022;Tiwari et al 2022). The SHRIMP U-Pb chronology of zircons from pelitic granulite, according to Prakash et al (2021), yields the ages between 780 Ma and 680 Ma as a period of metamorphic overprint, and the ages between 1591 Ma and 1216 Ma match well with detritus formed from a magmatic/ sedimentary source for pelitic granulite.…”

Section: Geodynamic Evolutionmentioning

confidence: 99%

“…(c) Geological map of the study area showing sample location (map modified after Srikarni et. al, 2004; Singh et al 2010; Prakash et al 2021; Biswal et al 2022). …”

Section: Introductionmentioning

confidence: 99%

“…Kishangarh nepheline syenite intruded at 1490 ± 150 Ma, while South Delhi Terrane (SDT) granites were also intruded at 1012 ± 78 Ma (Crawford, 1970). Additionally, due to deformations that occurred millions of years ago in the Aravalli-Delhi mountain ranges, the Sandmata rocks that are found along the terrane boundary have been bent (Naha & Halyburton, 1974; Sen, 1980; Srivastava, 2001; Bhowmik et al 2010; Singh et al 2010, 2020; Roy et al 2012, 2016; Tiwari & Biswal, 2019; Biswal et al 2022; Tiwari et al 2022). Therefore, the older ages of the Mangalwar and Sandmata complexes are reset to younger ages, particularly in the northern part of the Banas shear zone (Bhowmik & Dasgupta, 2012; Ahmad & Mondal, 2016; Kumar et al 2019; D’Souza et al 2021).…”

Section: Introductionmentioning

confidence: 99%

“…Therefore, the older ages of the Mangalwar and Sandmata complexes are reset to younger ages, particularly in the northern part of the Banas shear zone (Bhowmik & Dasgupta, 2012; Ahmad & Mondal, 2016; Kumar et al 2019; D’Souza et al 2021). It is generally agreed that the collision between the Bundelkhand craton and the Marwar craton was the primary driving force behind the orogeny that resulted in the development of the ADMB (Bhowmik et al 2010; Singh et al 2010, 2020; Tiwari & Biswal, 2019; Biswal et al 2022; Tiwari et al 2022).…”

Section: Introductionmentioning

confidence: 99%

“…Pelitic granulite found in the region have a structure similar to gneiss and are composed of minerals that are organized into coarse bands of varying shades of light and dark colours having characteristic minerals such as spinel, cordierite, garnet, sillimanite, hypersthene, feldspar, quartz, biotite and plagioclase. The lighter bands are composed of quartzo-feldspathic material, while the darker bands are predominantly composed of cordierite and contain reddish brown garnets scattered/dispersed throughout (Bhowmik et al 2010; Singh et al 2010, 2020; Tiwari & Biswal 2019; Prakash et al 2021; Biswal et al 2022; Tiwari et al 2022).…”

Section: Introductionmentioning

confidence: 99%

See 4 more Smart Citations

“Geochronology and geochemistry of pelitic granulite from the South Delhi Terrane of the Aravalli Delhi Mobile Belt, NW India: implications for petrogenesis and geodynamic model”

et al. 2023

View full text Add to dashboard Cite

An attempt has been made to illustrate the evolution of pelitic granulite from south of the Balaram-Abu road, which lies in the South Delhi Terrane (SDT) of the Aravalli-Delhi Mobile Belt (ADMB), using geochemistry and geochronology. The current work offers a plausible explanation for the protolith of pelitic granulite, nature of the sediments and its provenance. The elemental geochemistry of the pelitic granulites reveals that the protolith is an arkosic to shaley type. The rare earth elements pattern shows that there is a negative Eu anomaly and a small excess of LREE over HREE. This means that the source of sediments probably has the same elements as the upper crust. However, the amounts of Sr, Nd and Pb vary a lot, which shows that the sediments supplied from two different types of sources (felsic and mafic) in different proportions from a Proterozoic terrain. The monazite geochronology indicates that the metamorphic overprint occurred between 797 Ma and 906 Ma. Additionally, the ages correlate to the debris that was formed between the 1188 Ma and 1324 Ma from magmatic/sedimentary sources for pelitic granulite. The present research provides a more in-depth understanding of the evolutionary history of the pelitic granulite that comprises the SDT in the ADMB region during the Proterozoic era.

show abstract

Section: Geodynamic Evolutionmentioning

confidence: 99%

“…(c) Geological map of the study area showing sample location (map modified after Srikarni et. al, 2004; Singh et al 2010; Prakash et al 2021; Biswal et al 2022). …”

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

See 3 more Smart Citations

“Geochronology and geochemistry of pelitic granulite from the South Delhi Terrane of the Aravalli Delhi Mobile Belt, NW India: implications for petrogenesis and geodynamic model”

et al. 2023

View full text Add to dashboard Cite

show abstract

Tracing source and palaeo‐weathering conditions of quartzose sandstone in the Cretaceous Cambay Basin: A combined petrographical, geochemical and geochronological approach

Rajak,

Prabhakar,

Banerjee

2023

Geological Journal

View full text Add to dashboard Cite

Based on detrital monazite dating, mineral chemistry of tourmaline and rutile, bulk rock geochemistry, modal analysis of petrographic and palaeocurrent data, this study tracks the source of quartzose sandstone within the Cretaceous succession of the Cambay Basin primarily to rocks within the Aravalli‐Delhi Fold Belt. Monazite geochronology shows predominant peaks around 506 ± 11 Ma, 905 ± 12 Ma and a minor peak at 750 ± 20 Ma, 1485 ± 30 Ma relating sediment sources to the Aravalli‐Delhi orogeny and Pan‐African orogeny. The petrographic modal analysis of the moderate‐to‐well‐sorted Himmatnagar Sandstone indicates at least 91% quartz, with minor feldspar and rock fragments. The mineral chemistry of tourmalines in Himmatnagar Sandstone matches with Li‐ and Ca‐poor granitoid, pegmatites, metapelites and quartz tourmaline rocks. The trace element content of rutiles in sandstones corresponds to metapelitic sources. Detrital monazite dates and mineral chemistry of tourmalines and rutiles pinpoint the sediment source to the South Delhi Supergroup of rocks. The dominance of rounded zircons and tourmalines and abraded quartz overgrowth in the Himmatnagar Sandstone indicate the recycling of sediments, possibly from the Marwar Supergroup. Palaeoclimatic proxies based on mineralogy and geochemistry, particularly, the high value (93–97) of mineralogical index alteration, indicate intense chemical weathering of the source rocks under humid climatic conditions. Therefore, the combination of factors, including the quartzo‐feldspathic source rocks, intense chemical weathering under humid climatic conditions and the recycling of sediments facilitated the formation of quartzose sandstone within the Himmatngar Sandstone in the Cambay Basin.

show abstract

Precambrian geology of India

Mazumder

Arima

2023

Earth-Science Reviews

View full text Add to dashboard Cite

A review on deformation structures of different terranes in the Precambrian Aravalli-Delhi Mobile Belt (ADMB), NW India: Tectonic implications and global correlation

Cited by 10 publications

References 101 publications

“Geochronology and geochemistry of pelitic granulite from the South Delhi Terrane of the Aravalli Delhi Mobile Belt, NW India: implications for petrogenesis and geodynamic model”

“Geochronology and geochemistry of pelitic granulite from the South Delhi Terrane of the Aravalli Delhi Mobile Belt, NW India: implications for petrogenesis and geodynamic model”

Tracing source and palaeo‐weathering conditions of quartzose sandstone in the Cretaceous Cambay Basin: A combined petrographical, geochemical and geochronological approach

Precambrian geology of India

Contact Info

Product

Resources

About