India Asia Research Articles

Palaeomagnetic indication for India–Asia collision at 12°N and maximum 810 km Greater India extent in the western suture zone

SUMMARY Knowing the pre-collisional extent of the northern Indian Plate margin (‘Greater India’) is vital to understanding the tectonic evolution of the India–Asia collision and the formation of the Himalayan–Tibetan orogen. However, suitable geological units for palaeomagnetic investigations along the Himalayan belt are limited, which makes it difficult to reconstruct Greater India during the pre-collisional period in Late Cretaceous to Palaeogene. Often the palaeomagnetic results from the Zongpu Formation at Gamba in southern Tibet (∼88.5°E) were used for estimates of Greater India, but their validity was recently questioned. As a contribution to closing the data gap, we performed a palaeomagnetic study of the Palaeocene/Lower Eocene Dibling limestone (DL) in the western Tethyan Himalaya of Zanskar (34.0°N/76.6°E). The results from 27 sites revealed a well grouping (k = 71.7) syntectonic magnetization with best grouping at 52 per cent unfolding. The remagnetization of the DL was acquired shortly after ∼54 Ma, at the latest at ∼49 Ma, and is probably carried by fine-grained magnetite formed during the early orogenic phase. Assuming proportional tilting of the fold limbs, the corresponding palaeolatitude of 11.8 ± 2.4°N suggests a maximum Greater India extent of 810 ± 420 km and a first continental contact with the southern Eurasian margin at ∼12°N in the western part of the suture zone. The tectonostratigraphic equivalence of the DL with the Zongpu Formation at Gamba and a great similarity in their magnetic properties supports a secondary origin of the Gamba results. Through understanding the mechanism of remagnetization in the DL, an early orogenic remanence acquisition is also indicated for the Zongpu Formation, and thus the Gamba results deserve further credit for Greater India reconstructions. However, we note a large inconsistency of the available Late Cretaceous and Palaeogene palaeolatitude data from the Tethyan Himalaya by up to ∼20°, corresponding to differences of up to ∼2000 km in the size of Greater India. These discrepancies require further palaeomagnetic work in the Tethyan Himalaya, and in particular we recommend comparative studies at same locations and of same units.

Kirloskar Brothers wins ethical company award

Kirloskar Brothers Ltd (KBL) has won CMO Asia's India's Most Ethical Company award in the Ethical Company in Industrial Manufacturing category.

Trade of the Portuguese Royal and Private Traders in India from the 16th to the 19th Century

The 16th–19th centuries was the period that witnessed the ups and downs development of the trade of the Portuguese Crown and the Portuguese private traders in India. In fact, the maritime trade of the Portuguese Crown only developed significantly in the 16th century; from the 17th century, because of different reasons, it declined gradually. Finally, it had to depend on the British at the end of the 19th century. In contrast with the Portuguese Crown trade, although the commerce of the Portuguese private merchants had to face a lot of difficulties, it continued to expand its role and influence during the four centuries (16th–19th). This article summarizes the trade of Portuguese royal and Portuguese private commercial activities in India from the 16th to the 19th century. On that basis, the authors of this article analyze and point out the core characteristics which fully and comprehensively reflect the development of commercial activities of the Portuguese royal family and merchants in India during this period. To conduct this research, the authors rely on the research results of scholars around the world directly or indirectly related to this issue and use two main research methods of Historical Science, including the historical method and the logical method. In addition, the authors also use several other research methods such as analysis, synthesis, statistics, and comparison. The completion of this study will make a scholarly contribution by helping researchers to have a more comprehensive and in-depth view of Portugal’s commercial activities in Asia in general and India in particular from the 16th to the 19th century.

Coastal Shrines and Transnational Maritime Networks Across India and Southeast Asia by Himanshu Prabha Ray

Coastal Shrines and Transnational Maritime Networks Across India and Southeast Asia by Himanshu Prabha Ray

Миграции из Южной Азии в Западную Европу: истоки, тенденции, перспективы

The article is concentrated on the phenomenon of Indian and South Asian migration to the countries of Western Europe. Initially, migration flows from this region were an inalienable part of metropolis–colonies interrelationship and were sustained on the notion of free and unrestricted movement of human resources from South Asia to the British Isles. After the dissolution of the British Empire and gaining independence, the inhabitants of India and South Asia, in search for a “happier life” overseas, set their course for the United Kingdom and Western Europe, where later migrants were put under rigorous political control. However, the flows of those seeking economic prosperity and political asylum remained intensive and became subject to methodical social regulations in Western Europe. Equilibrium of this kind was put to a severe test when the migration crisis of 2015 and 2016 broke out. Only the most advanced groups of migrants could adjust themselves to the newly emerged reality as demonstrated by the cases of the Netherlands and Italy. The Dutch government has restricted the inflow of low-skilled labour, while encouraging skilled immigration. Indian labour force is generally employed in IT, consultancy, engineering or management. Local and national governments work together with private partners to make the lives of these newcomers easier. High-skilled migrants are welcome as new citizens. Most Indians in Italy have settled in the north of the country and work in agriculture. Indians are considered industrious, business-minded, hard-working and law-abiding. The Indian migrant community has integrated successfully into Italian economic and social life. The author argues that the Dutch and Italian practice of handling the Indian migrants could be critically absorbed in Russia that is keen to attract the “demographic dividend” from outside.

Temporal and Spatial Variations of Enriched Source Components in Linzizong Volcanic Succession, Tibet, and Implications for the India–Asia Collision

Abstract The temporal and spatial distribution of enriched source components at sites of continent–continent collision provides critical insights into mantle dynamic processes associated with subduction- and collision-related events. However, determining the origin of such enriched components remains a significant challenge. We report a comprehensive dataset of the Linzizong volcanic succession (LVS) from four locations with varying distance across-strike to the Indus–Yarlung suture in southern Tibet, which marks the exposed surface expression of the India–Asia collision zone. The LVS rocks in this study can be divided into two groups: a calc-alkaline Group 1 (69–55 Ma), mainly including basaltic–andesitic varieties, and a shoshonitic Group 2 (52–50 Ma), consisting predominantly of silicic rocks with minor mafic compositions. Group 1 samples are likely derived from the fractional crystallization of primitive basaltic melts as a result of the partial melting of a metasomatized mantle wedge. These samples are decoupled in Nd–Hf isotopic compositions, suggesting an incorporation of subducting sediment-derived melts into the mantle wedge. The influence of sediment-derived melt on the mantle source increases away from the suture zone toward Asia (i.e., from the south to the north) as indicated by the more enriched Sr, Nd, Pb, and Hf isotopic compositions, as well as elevated Th/La and La/Sm ratios. The heavy δ26Mg values, and high Ba/Th and Sr/Th ratios of samples close to the suture coincide with the dehydration of the subducting Neo-Tethyan slab. Group 2 mafic samples have depleted and coupled εNd–εHf isotopic compositions and are characterized by elevated (La/Yb)N and Dy/Yb ratios as well as low Zr/Nb ratios, indicating an origin of enriched garnet-bearing lithospheric mantle with contributions from asthenosphere-derived materials. Group 2 silicic samples are isotopically enriched both near and far away from the suture, which can be attributed to the involvement of ancient lower crust-derived melt from Tethyan Himalaya and central Lhasa subterrane basement, respectively. Our results show that the LVS are the magmatic response to late subduction (Group 1), and to initial India–Asia collision and slab breakoff (Group 2). Negative trends in the whole-rock Nd and zircon Hf isotopic compositions at ~51 Ma should be treated with caution for geodynamic interpretations, depending on the distance between the samples and the India–Asia suture.

Mesozoic–Cenozoic Uplift/Exhumation History of the Qilian Shan, NE Tibetan Plateau: Constraints From Low-Temperature Thermochronology

The Qilian Shan, which is located along the northeastern margin of the Tibetan Plateau, plays a key role in understanding the dynamics of the outward and upward growth of the plateau. However, when and how tectonic deformation evolved into the geographic pattern which is currently observed in the Qilian Shan are still ambiguous. Here, apatite fission track (AFT) thermochronology and sedimentology were conducted to interpret the low-temperature tectonic deformation/exhumation events in well-dated Late Miocene synorogenic sediment sequences in the Xining Basin, which is adjacent to the southern flank of the Qilian Shan. These new low-temperature thermochronological results suggest that the Qilian Shan experienced four stages of tectonic exhumation during the late Mesozoic–Cenozoic. The Late Cretaceous exhumation events in the Qilian Shan were caused by the diachronous Mesozoic convergence of the Asian Plate and Lhasa Block. In the early Cenozoic (ca. 68–48 Ma), the Qilian Shan quasi-synchronously responded to the Indian–Asian plate collision. Subsequently, the mountain range experienced a two-phase deformation during the Eocene–Early Miocene due to the distal effects of ongoing India–Asia plate convergence. At ca. 8 ± 1 Ma, the Qilian Shan underwent dramatic geomorphological deformation, which marked a change in subsidence along the northeastern margin of the Tibetan Plateau at that time. Our findings suggest that the paleogeographic pattern in the northeastern Tibetan Plateau was affected by the pervasive suture zones in the entire Qilian Shan, in which the pre-Cenozoic and Indian–Asian plate motions reactivated the transpressional faults which strongly modulated the multiperiodic tectonic deformation in northern Tibet during the Cenozoic. These observations provide new evidence for understanding the dynamic mechanisms of the uplift and expansion of the Tibetan Plateau.

Detrital Zircon Provenance of the Cenozoic Sequence, Kotli, Northwestern Himalaya, Pakistan; Implications for India–Asia Collision

This study reported the detrital zircon U-Pb geochronology of the Cenozoic sequence exposed in Kotli, northwestern Himalaya, Pakistan, which forms part of the Kashmir foreland basin. The U-Pb detrital age patterns of the Paleocene Patala Formation show a major age cluster between ~130–290 Ma, ~500–1000 Ma and ~1000–1500 Ma, which mainly resembles the lesser and higher Himalayan sequence. However, the younger age pattern (~130–290 Ma) can be matched to the ages of the ophiolites exposed along the Indus–Tsangpo suture zone. In addition, two younger grains with 57 Ma and 55 Ma ages may indicate a contribution from the Kohistan-Ladakh arc. The detrital zircons in the upper Tertiary sequence show the increased input of younger detrital ages <100 Ma, with more pronounced peaks at ~36–58 Ma, ~72–94 Ma and ~102–166 Ma, indicating the strong resemblance to the Asian sources including the Kohistan–Ladakh arc, Karakoram block and Gangdese batholith. This provenance shift, recorded in the upper portion of Patala Formation and becoming more visible in the upper Tertiary clastic sequence (Kuldana and Murree formations), is related to the collision of the Indian and Asian plates in the northwestern Himalayas. Considering the age of the Patala Formation, we suggest that the Indian and Asian plates collided during 57–55 Ma in the northwestern Himalayas, Pakistan.

Human Capital vs. Quality of Life: A Sociological Appraisal

The present article sociologically analyzes how human capital and quality of life mutually affect each other. Yet, human capital is strongly possible in changing quality of life. Most countries first try to build their human capital, to be followed by a better and more prosperous quality of life. For example, South Korea and India in Asia have initially upgraded their human capital which was followed by improvement in quality of life in various sectors. In fact, in all societies, educated men and women generally have lower mortality rates; their offspring also have higher survival rates. Thus, the educational capital that leads to social capital, while affecting the current generation, also has a positive effect on future generations. Almost globally, women with higher levels of education have fewer children. They have better access to birth control tools. Such a quality of life further leads to the continuity of future quality of life. Improved quality of life leads to food per capita, accommodation per capita, services per capita, convenience per capita, and many more.

Northward Growth of the West Kunlun Mountains: Insight From the Age–Elevation Relationship of New Apatite Fission Track Data

The Cenozoic collision between India and Asia promoted the widespread uplift of the Tibetan Plateau, with significant deformation documented in the Pamir Plateau and West Kunlun Mountains. Low-temperature thermochronology and basin provenance analysis have revealed three episodes of rapid deformation and uplift in the Pamir–West Kunlun Mountains during the Cenozoic. However, there is very little low-temperature thermochronology age–elevation relationship (AER) data on fast exhumation events in this area—especially in the West Kunlun Mountains— leading to uncertainty surrounding how these events propagated within and around the mountain range. In this study, we produced an elevation profile across granite located south of Kudi, Xijiang Province, China, to reveal its exhumation history. Apatite fission track AER data show that a rapid exhumation event occurred at ∼26 Ma in the southern West Kunlun Mountains. When combined with published data, we interpret that the initial uplift events related to the India–Asia collision began in the central Pamir, southern West Kunlun, and northern West Kunlun regions during the Late Eocene, Oligocene, and Middle Miocene periods, respectively. Therefore, the Cenozoic northward growth process occurred from south to north around West Kunlun.

Subducted sediment contributions to REE deposits recorded by alkaline mafic dikes in the Lizhuang REE deposit, Panxi area, southwest China

Carbonatite-associated rare earth element (REE) deposits are the most important source of REEs worldwide. Recycled subducted sediments are critical for REE mineralization, but it remains unclear how the subducted sediments contribute to the REE mineralization. This study presents new whole-rock and apatite geochemical data for alkaline mafic dikes from the Lizhuang REE deposit, southwest China. These alkaline mafic dikes were emplaced at ca. 28.4 Ma (monazite U-Pb age), broadly coeval with the carbonatite–syenite complex and REE mineralization in the Lizhuang REE deposit. The alkaline mafic dikes have enriched Sr-Nd-Pb isotopic compositions, and variable Ba/Th and La/Sm ratios, demonstrate they were derived from an enriched mantle source, which had been modified by both slab-derived fluids and sediment melts. The apatite grains in the alkaline mafic dikes have distinctive geochemical features in their irregular cores (apatite A) and rim overgrowths (apatite B). Apatite A has low REE contents (18.6–161 ppm) and apatite B has high REE contents (1869–4288 ppm). The different REE contents in these apatites could have been caused by the addition of REE-rich carbonatitic melts at lower crustal depths. We propose that the REE-rich carbonatitic melts could be formed by melting of a sediment-rich mantle source, and that collision between India–Asia triggered the melting.

Early mesozoic arc–back-arc system in the leading edge of the Tibetan Plateau

The southern Lhasa subterrane is the leading edge of the Tibetan Plateau and preserves important records of the Neo-Tethyan oceanic subduction and India–Asia collision. However, the early tectonic evolutionary history of the Neo-Tethyan oceanic subduction remains unclear. Here we present results from a systematic study on the early Mesozoic (Middle Triassic–Late Jurassic) magmatic and sedimentary rocks in the southern Lhasa subterrane. These rocks are distributed zonally along the southern and northern parts of the subterrane, and have been classified into the north and south belts. The magmatic rocks in the north belt show a back-arc basin affinity, with accreted bimodal volcanic sequence and sediments from central and southern Lhasa subterranes, whereas the magmatic rocks in the south belt reveal typical magmatic arc characteristics. The sediments were derived from southern Lhasa subterrane, without the input of clastic components from the central Lhasa subterrane. Based on geochronological, geochemical, and sedimentary records from both belts, we conclude that the early Mesozoic magmatism was triggered by the northward subduction of the Neo-Tethyan oceanic slab, and its initial subduction likely occurred before the Middle Triassic (ca. 240 Ma). During the Early–Middle Jurassic (ca. 193–165 Ma), a short-lived episode of back-arc extension, we attribute to roll-back of the subducting Neo-Tethyan slab, resulted in the single magmatic arc that existed during the early stages (ca. 240–194 Ma) and evolved gradually into an arc–back-arc system. The north belt represents a back-arc basin setting associated with a continental arc, whereas an intra-oceanic and continental (island) arc simultaneously developed in the south belt, and both these belts were possibly generated under the same subduction system.

Crustal reworking and growth during India–Asia continental collision: Insights from early Cenozoic granitoids in the central Lhasa Terrane, Tibet

Studying granitoids can provide important knowledge on the composition of continental crust and the geodynamic processes of continental growth. Nevertheless, the mechanisms of granitoids formation during continental collision remain uncertain. In this paper, we present new zircon U–Pb–Hf isotope and whole‐rock Sr–Nd isotope compositions, and major‐ and trace‐element data for granitoids from the Chacangka area of the central Lhasa Terrane, southern Tibet. The Chacangka quartz monzonites crystallized at ca. 61 Ma, whereas the monzonites and granites were emplaced at ca. 51 Ma. The quartz monzonites are peraluminous and have high 87Sr/86Sri ratios (0.7129–0.7131), and their low εNd(t) (−7.65 to −7.10) and zircon εHf(t) (−9.3 to −7.5) values are more depleted than those of ancient crustal basement beneath the central Lhasa Terrane, which suggests that they originated from a mixed source of juvenile and ancient lower crust. Compared with the quartz monzonites, the monzonites have much higher contents of MgO (2.34–3.62 wt%) and values of Mg# (42.3–46.3) and zircon εHf(t) (−6.9 to 1.9) and show more depleted Sr–Nd isotopes, indicating that more juvenile materials were involved in their source. The granites have Sr–Nd isotope compositions that are similar to those of the coeval monzonites but have higher SiO2 contents, lower CaO and MgO contents, and lower values of Mg#, suggesting that they were differentiates of the monzonites. The elemental and isotopic compositions of the Chacangka granitoids exhibit a marked transformation from 61 to 51 Ma, probably indicating breakoff of the Neo‐Tethyan oceanic slab. The Neo‐Tethyan slab breakoff not only induced the upwelling of deep material and eruption of magma but also caused re‐melting and destruction of ancient crustal basement of the central Lhasa Terrane.

Crustal thickening versus lateral extrusion during India–Asia continental collision: 3-D thermo-mechanical modeling

Continental collision between the Indian and Eurasian plates in the past ~55 ± 5 Ma has led to the development of the Tibetan Plateau, where nearly doubled crustal thickness indicates intense lithospheric thickening during the collision. On the other hand, geological evidence indicates significant lateral extrusion of Tibetan materials around the edges of the plateau, especially around the Eastern Himalaya Syntaxis. Two end-member models, “pure shear thickening” and “tectonic escape”, emphasize respectively the vertical and lateral deformation of Tibetan lithosphere during the collision. However, their competing roles in accommodating the Tibetan continental collision remain debated. Here, we developed a series of 3-D high-resolution numerical models to systematically study strain partitioning between crustal thickening and lateral extrusion during the collision. The model focuses on eastern Tibetan Plateau, where most of the escaping tectonics occurred. The model results indicate that the amount of crustal thickening is generally several times higher than that of lateral extrusion in accommodating the lithosphere shortening. The partitioning between crustal thickening and lateral extrusion depends on the rheological contrast between the Tibetan and neighboring blocks, whereas the relic suture zones within the Tibetan lithosphere do not control the strain partitioning but affect the morphology. The southward motion of the Indochina block, resulting from extension caused by trench retreating, has major impacts on the development of large-scale lateral extrusion tectonics. The vertical variation of lithospheric rheology leads to faster motion of the crust than the mantle lithosphere in the extruding block, hence mechanical decoupling between the extruding crust and lithospheric mantle.

Tectonic discontinuity, partial melting and exhumation in the Garhwal Himalaya (Northwest India): Constrains from spatial and temporal pressure-temperature conditions along the Bhagirathi valley

The pattern and timing of tectonic discontinuity and partial melting in the Garhwal Himalaya, resulting from the India–Asia collision, are crucial factors for understanding the evolution of the Himalayan orogen, but these parameters remain poorly constrained. Middle- to high-grade metamorphic rocks from the Main Central Thrust (MCT) zone and the High Himalaya Crystalline Sequence (HHCS) along the Bhagirathi valley in northwest India have been investigated in this study. The primary mineral assemblage of the gneisses and migmatites in the HHCS is garnet + biotite + white mica + quartz + kyanite + rutile ± ilmenite ± sillimanite. The metamorphic grade at thermal peak rapidly increases upwards across the MCT from garnet schists (515–550 °C, 8–9 kbar) in the footwall to garnet-bearing migmatite (705–735 °C, 10–13 kbar) in the hanging wall. The P–T condition decreased upwards in kyanite gneiss of the lower HHCS (690 °C, 8.3 kbar), yielding a high field pressure gradient near the MCT. The prominent metamorphic discontinuity could have been caused by the southward extrusion of the HHCS along with the MCT. The base of the HHCS experienced high-grade metamorphism at 38–25 Ma, mainly at 31.9 ± 0.5 Ma. The new data, combined with previous studies, suggest that the prominent metamorphic discontinuity is characterized by the different periods of peak metamorphism and the overprint in the hanging wall (Eocene–Oligocene metamorphism and Early Miocene overprint) and footwall (Early Miocene metamorphism and Late Miocene to Pliocene overprint) of the MCT. The second metamorphic discontinuity occurred near the migmatite zone in the lower-middle HHCS, which experienced the anatexis (690–740 °C, 7–9 kbar) at 37–25 Ma, mainly at 33.9 ± 1.2 Ma. The Bhagirathi HHCS experienced a regional Barrovian-type Eohimalayan metamorphism associated with fluid-present melting of muscovite + plagioclase + quartz + H2O → melt ± kyanite at 34–32 Ma without a strong Miocene overprint. The period of partial melting is significantly older than the intrusion of ca. 22 Ma Early Miocene Gangotri leucogranites at the top of the HHCS. Protracted periods of crystallization (38–22 Ma) indicate a long duration of more than ca. 15 Myr of anatexis, from initiation of migmatization to pluton formation in the Bhagirathi HHCS. The protracted fluid-present melting and subsequent rapid exhumation in the Bhagirathi HHCS could be associated with heterogeneous extrusion forming the tectonic discontinuity in the lower-middle HHCS. The metamorphic grade decreased towards the upper HHCS (620 °C, 6.5 kbar) across the Jhala Normal Fault where occurs in the right-way-up sequence. On the other hand, in the central Himalaya, the thrusting occurred between upper HHCS and lower-middle HHCS in the inverted metamorphic sequence. The Early Miocene migmatites in the footwall of the significant tectonic discontinuity are dominant, and diachronous extrusion accompanied with the fluid-absent melting reactions is the common mechanism to exhume the HHCS, unlike the heterogeneous extrusion in the northwest Himalaya.

​Cloning and Sequence Analysis of Transferrin Binding Protein Gene A of Field and Vaccine Strains of Pasteurella multocida B:2

Background: Pasteurella multocida is an important bacterial pathogen that causes many major diseases of which haemorrhagic septiciemia (HS) in cattle and buffalo is responsible for catastrophic epizootics in India and South Asia. In India, the disease haemorrhagic septiciemia is considered as the most dreaded bacterial disease. Various host- and pathogen- specific determinants are responsible for disease outcome. Various bacterial virulence genes (tbpA, pfhA, toxA, hgbB, hgbA, nanH, nanB, sodA, sodC, oma87 and ptfA) have been proposed to play a key role in this interaction. Methods: The present study was done to compare the gene and deduced amino acid sequence of transferrin binding protein gene (tbpA) gene of field isolates and vaccine strain of P. multocida B: 2. Result: It was observed that tbpA gene of field and vaccine strains have similar nucleotide sequence except at positions 574 and 620. The sequence of tbpA gene was used for prediction of matured TbpA protein characteristics. The deduced amino acid sequences of 242 amino acids revealed 99% homology with TbpA of P. multocida and with a variety of other TonB-dependent receptor proteins, indicating that it belongs to the family of outer membrane receptors. Deduced amino acid sequence was found to be similar in field and vaccine strains except at 207th amino acid. In field isolates Leucine was there while in vaccine strain Phenyl alanine was found. These both amino acids are hydrophobic in nature so no change in physico-chemical property of TbpA is expected. From this study it is concluded that single amino acid difference between field isolate and vaccine strain might not cause change in its binding and physico-chemical property.

Situation on the Global Coal Market during the Recovery of the World Economy after the COVID-19 Crisis

The global economic recovery in 2021 will lead to a recovery in coal demand after a significant drop in 2020 caused by the Covid-19 crisis. There is no indication that the global coal consumption will decline significantly in the coming years, as increased demand in some Asian countries will offset declines in others. Based on the assumption of a global economic recovery, experts forecast a 2.6% growth in the global coal demand in 2021, driven by an increased demand for electricity and industrial production. The economies of China, India and Southeast Asia account for most of the growth. The future of coal will largely be decided in Asia. Today, China and India account for 65% of the world's coal demand. Taking into account Japan, Korea, Taiwan and Southeast Asia, this share rises to 75%. China will be particularly influential, as it currently accounts for half of the world's coal consumption. By 2025, the European Union and the United States will account for less than 10% of global coal demand, down from 37% in 2000.

Petrology and geochemistry of ultramafic rocks in the Mogok belt, Myanmar: Cumulates from high‐pressure crystallization of hydrous arc melts

The Mogok metamorphic belt (MMB) in central Myanmar is well known for its complex tectonics, magmatism, and metamorphism in the framework of Tethyan subduction and India–Asia collision. It is also world renowned due to the gemstone‐class rubies and sapphires. Identification and discrimination of those petrological units in this region therefore are important for understanding the gemstone mineralization. Ultramafic massifs also crop out together with the gemstone‐bearing metamorphic rocks in the MMB. It is still poorly constrained about their origin (i.e., mantle peridotites of Jurassic–Cretaceous ophiolites or cumulate rocks) and their relationship with the gemstone generation. Here, we report petrological and geochemical data for the Mogok ultramafic rocks. Petrographic observations show that they have typical cumulate textures, with a crystallization order of olivine/spinel‐orthopyroxene‐clinopyroxene. They have low whole‐rock Al2O3 and CaO, and extremely high spinel Cr# (=Cr/[Cr + Al]; up to 0.86). Clinopyroxenes of these rocks show light rare earth element enriched patterns when normalized to CI chondrite. The results suggest that the Mogok ultramafic rocks have different compositions, both whole‐rock and mineral, from mantle peridotites of Myanmar ophiolites, such as the Kalaymyo and Myitkyina ophiolites, but resemble typical Alaskan‐type ultramafic cumulates. Therefore, the Mogok ultramafic rocks are cumulates generated by high‐pressure crystallization of hydrous arc melts, probably during the subduction of the Tethyan oceanic slab. We argue that the emplacement of these arc melts may have provided additional heat for the earlier magmatic rocks and regional high‐temperature metamorphism, although there is a need to further constrain the ages of these rocks. This, along with magmatism and metamorphism during post‐collisional extension, probably collectively contributed to the generation of world‐class coloured gemstone mineralization.

Active Strike-Slip Faulting and Systematic Deflection of Drainage Systems along the Altyn Tagh Fault, Northern Tibetan Plateau

Systematic deflection of drainage systems along strike-slip faults is the combination of repeated faulting slipping and continuous headward erosion accumulated on the stream channels. The measurement and analysis of systematically deflected stream channels will enhance our understanding on the deformational behaviors of strike-slip faults and the relationship between topographic response and active strike-slip faulting. In this study, detailed interpretation and analysis of remote sensing images and DEM data were carried out along the Altyn Tagh Fault, one typical large-scale strike-slip fault in the northern Tibetan Plateau, and together with the statistical results of offset amounts of 153 stream channels, revealed that (i) the drainage systems have been systematically deflected and/or offset in sinistral along the active Altyn Tagh Fault; (ii) The offset amounts recorded by stream channels vary in the range of 7 m to 72 km, and indicate a positively related linear relationship between the upstream length L and the offset amount D, the channel with bedrock upstream generally has a better correlation between L and D than that of non-bedrock upstream; (iii) River capture and abandonment are commonly developed along the Altyn Tagh Fault, which probably disturbed the continuous accumulation of offset recorded on individual stream channel, suggesting that the real maximum cumulative displacement recorded by stream channels might be larger than 72 km (lower bound) along the Altyn Tagh Fault. Along with the cumulative displacements recorded by other regional-scale strike-slip faults in the Tibetan Plateau, these results demonstrate that the magnitude of tectonic extrusion along these first-order strike-slip faults after the collision of India–Asia plates might be limited.

Mongolia’s assertive and pragmatic role in India’s Connect Central Asia Policy: Current trajectory and Future Ahead

Mongolia’s uniqueness and importance in contemporary world politics lie in its geographical situating, demography, and economy. Geographically landlocked and situated in the Eurasian intersection, Mongolia has the lowest population density of any sovereign country on the planet. Sandwiched among Russia and China Mongolia's harsh environment limit its economic interests. However, Mongolia's geostrategic position, unexplored energy assets, and democratic governance have expanded its importance in global politics. Because of such Mongolia holds a key position in India's Act East and Connect Central Policy to counter China's expansionist policies in North-East Asia. With regards to India-Mongolia relations, the two nations share a rich historical legacy. Tibetan Buddhism the most prevailing religion in Mongolia makes social linkages, Democracy solidified further connections between India and Mongolia. Because of these old and profoundly established linkages, India-Mongolia are 'spiritual neighbors'. However, China still has an overreaching control over Mongolia’s trade, commerce, and other sectors. China also dominates intra-regional trade in North-East Asia. Under India’s Connect Central Asia India attempts to counter Chinese encirclement by delving into close strategic, economic, and energy relations with China's neighbors like Mongolia and CAS. However, the achievement or failure of India's Connect Asia Policy will depend upon India's political as well as its diplomatic will to transform India's interest in regional integration in reality.