The main purpose of the present research is to study geological issues of urban areas in Bagh-e Malek in Khuzestan province of Iran and improving the municipal environment. The present research is an applied study in ...The main purpose of the present research is to study geological issues of urban areas in Bagh-e Malek in Khuzestan province of Iran and improving the municipal environment. The present research is an applied study in sake of nature and a descriptive-analytical survey in sake of method. Library and field method has been used in data collection. In field study, 325 citizens in Bagh-e Malek in 2015 were selected as sample group via sampling method well suited to sample size using questionnaire of citizens’ participation. Software SPSS and Excel are used to analyze data. Friedman test has been used to determine rank of each of selected indices for testing hypotheses and finding research. Results from Friedman test indicate that satisfaction with pedestrian passages has the highest mean with rank (9.90) and awareness from municipality’s rights has the lowest mean with rank (2.95).展开更多
Enhanced weathering(EW)of ultramafi c rocks from the Muslim Bagh Ophiolite,Pakistan,has been studied in laboratory experiments to explore carbon sequestration as a climate change mitigation strategy for coastal and op...Enhanced weathering(EW)of ultramafi c rocks from the Muslim Bagh Ophiolite,Pakistan,has been studied in laboratory experiments to explore carbon sequestration as a climate change mitigation strategy for coastal and open sea environments.The research focused on a cost-eff ective ex situ experiment to examine the eff ects of EW reaction pathways arising from the interactions among rock powder,seawater and CO_(2).The experimental fi ltrates from diff erent milled peridotite samples exhibit a decrease in the Mg/Ca ratio as the specifi c surface area increases,which accelerates reaction rates.This suggests that the leached Mg from the original rock may have been consumed in the formation of brucite,serpentine and carbonates during EW.Similar reaction pathways are also responsible for the chemical alterations observed in amphibolite,albeit to varying degrees.On the other hand,the experimental residues showed an increase in loss on ignition compared to the original rock,indicating that EW has facilitated the incorporation of H 2 O and CO_(2) into secondary mineral structures through various reaction pathways,leading to the formation of brucite,serpentine and carbonates.Thermal gravimetric analysis of the experimental residues confi rms the presence of these minerals based on their decomposition temperatures.Additionally,XRD analysis identifi ed a range of carbonates in the residues of both peridotite and amphibolite samples,validating the occurrence of carbonation reactions.SEM images reveal textural changes in both samples,supporting the formation of secondary minerals through EW,consistent with observations from the petrographic study of untreated samples.Control experiments on CO_(2) absorption in seawater showed a decrease in pH,highlighting ocean acidifi cation from increased CO_(2) emissions.However,when rock powder was added to the seawater-CO_(2) mixture,the pH increased.This suggests that the EW of ultramafi c rock powders can sequester CO_(2) while raising seawater pH through the formation of secondary minerals.This research could serve as an analog for EW applications,considering the worldwide abundance of ultramafi c rocks and the availability of coastal and open ocean environments.However,further research is required to understand the behavior of other elements and their impacts on ocean chemistry in EW processes before applying CO_(2) sequestration strategies.展开更多
The site of Mansehra is located seismically in an active regime, known as the Crystalline Nappe Zone and Hazara-Kashmir Syntaxis in NW Himalayas, Pakistan. Seismic Hazard Assessment （SHA） for the site has been carri...The site of Mansehra is located seismically in an active regime, known as the Crystalline Nappe Zone and Hazara-Kashmir Syntaxis in NW Himalayas, Pakistan. Seismic Hazard Assessment （SHA） for the site has been carried out by considering the earthquake source zones, selection of appropriate attenuation equations, near fault effects and maximum potential magnitude estimation. The Mansehra Thrust, Oghi Fault, Banna Thrust, Balakot Shear Zone, Main Boundary Thrust, Panjal Thrust, Jhelum Fault and Muzaffarabad Fault and, further to the south, the Sanghargali, Nathiagali, and Thandiani Thrusts are the most critical tectonic features within the 50 km radius of Mansehra. Using the available instrumental seismological data from 1904 to 2007, SHA has been carried out. Other reactivated critical tectonic features in the area have been investigated. Among them the Balakot-Bagh fault, with the fault length of 120 km from Balakot to Poonch, has been considered as the most critical tectonic feature on the basis of geological/structural/seismological data. The potential earthquake of maximum magnitude 7.8 has been assigned to the Balakot-Bagh fault using four regression relations. The peak ground acceleration value of 0.25 g （10% probability of exceedance for 50 years） and 0.5 g has been calculated with the help of the attenuation equation using probabilistic and deterministic approaches.展开更多
An attempt has been made to systematically revise the Late Cretaceous （Turonian） bivalves of the Bagh Beds, central India. Altogether, fifteen species have been described here. The two species Nicaniella （N） trigo...An attempt has been made to systematically revise the Late Cretaceous （Turonian） bivalves of the Bagh Beds, central India. Altogether, fifteen species have been described here. The two species Nicaniella （N） trigonoides ＆ Protocardia （P） laticostata, which are earlier known from Late Cretaceous of Tiruchirapalli subbasin, southern India, have been recorded for the first time from Narmada Basin. The other species recorded are： Modiolus typicus, Neithea morrisi, Plicatula batnensis, P. numidica, P. instabilis, Lucina （L.） cf. fallax, Astarte similis, Opis corniformis, Protocardia hillana, P. madagascariense, Cytherea （Callista） lancianata, Trigonocallista spathi and Pholadomya sp.. During course of systematic revision, it has been found that many species described by earlier workers from the Late Cretaceous of Bagh Beds have been found conspecific to already known species from the Cretaceous of different parts of the globe and hence, they have been recorded here as junior synonyms. These species have immense implication in the palaeobiogeography of the region.展开更多
Rising sea-levels in tectonically active epicontinental basins often lead to varied depositional settings and palaeogeography, mostly influenced by the net accommodation resulting from mutual interference of the exten...Rising sea-levels in tectonically active epicontinental basins often lead to varied depositional settings and palaeogeography, mostly influenced by the net accommodation resulting from mutual interference of the extent and nature of landward encroachment by the sea and the net sedimentation. The Cenomanian Nimar Sandstone Formation, Bagh Group, Narmada rift basin, uniquely portrays the effect of sea-level rise within an intra-cratonic setting and attributes to the corresponding palaeogeographic changes in west-central India. An integrated sedimentological–sequence-stratigraphic study of the broadly fining-upward Nimar Sandstone Formation(thickness~ 20–30 m) depicts the actual nature of changeover from a fluvial to a marine-dominated transitional depositional setting. Detailed sedimentological study reveals total seventeen facies, grouped in five facies associations, viz., the channel-fill facies association(FA-1), the overbank facies association(FA-2), the fluvial-dominated fluvio-tidal facies association(FA-3), the tide-dominated fluvio-tidal facies association(FA-4), and the shoreface facies association(FA-5). Overall facies architecture indicates a west-to-eastward marine encroachment, resulting in stacking of three distinct palaeo-depositional conditions:(i) an initial fluvial system with channel and overbank, changing into a tideinfluenced fluvial bay-head delta in the inner estuary, followed by(ii) marine encroachment leading to a tidedominated central estuary with inter-to sub-tidal settings, and finally,(iii) with further intense marine encroachments, a wave-reworked open shore condition in the outer estuary zone. The overall fining-up succession with a systematic change from fluvial to marine-dominated depositional systems points to a landward shift of the shoreline, signifying a major transgressive event correlated to the Cenomanian global sea-level rise. Characteristic stratal stacking patterns point to four coarsening-and fining-up hemicycles, embedded within the major transgressive succession. These high-frequency cycles attest to the varied interplay of sedimentation, tectonics and sea-level changes, and the resultant net accommodations. A palaeogeographic model is proposed based on the high-frequency transgressive–regressive hemicycles, which envisages the evolution of the depositional environments in relation to the Cenomanian eustatic rise in the intra-cratonic riftogenic fluvio-marine transitional basinal setup.展开更多
文摘The main purpose of the present research is to study geological issues of urban areas in Bagh-e Malek in Khuzestan province of Iran and improving the municipal environment. The present research is an applied study in sake of nature and a descriptive-analytical survey in sake of method. Library and field method has been used in data collection. In field study, 325 citizens in Bagh-e Malek in 2015 were selected as sample group via sampling method well suited to sample size using questionnaire of citizens’ participation. Software SPSS and Excel are used to analyze data. Friedman test has been used to determine rank of each of selected indices for testing hypotheses and finding research. Results from Friedman test indicate that satisfaction with pedestrian passages has the highest mean with rank (9.90) and awareness from municipality’s rights has the lowest mean with rank (2.95).
基金supported by internal grant from Sultan Qaboos University(IG/DVC/ESRC/21/01).
文摘Enhanced weathering(EW)of ultramafi c rocks from the Muslim Bagh Ophiolite,Pakistan,has been studied in laboratory experiments to explore carbon sequestration as a climate change mitigation strategy for coastal and open sea environments.The research focused on a cost-eff ective ex situ experiment to examine the eff ects of EW reaction pathways arising from the interactions among rock powder,seawater and CO_(2).The experimental fi ltrates from diff erent milled peridotite samples exhibit a decrease in the Mg/Ca ratio as the specifi c surface area increases,which accelerates reaction rates.This suggests that the leached Mg from the original rock may have been consumed in the formation of brucite,serpentine and carbonates during EW.Similar reaction pathways are also responsible for the chemical alterations observed in amphibolite,albeit to varying degrees.On the other hand,the experimental residues showed an increase in loss on ignition compared to the original rock,indicating that EW has facilitated the incorporation of H 2 O and CO_(2) into secondary mineral structures through various reaction pathways,leading to the formation of brucite,serpentine and carbonates.Thermal gravimetric analysis of the experimental residues confi rms the presence of these minerals based on their decomposition temperatures.Additionally,XRD analysis identifi ed a range of carbonates in the residues of both peridotite and amphibolite samples,validating the occurrence of carbonation reactions.SEM images reveal textural changes in both samples,supporting the formation of secondary minerals through EW,consistent with observations from the petrographic study of untreated samples.Control experiments on CO_(2) absorption in seawater showed a decrease in pH,highlighting ocean acidifi cation from increased CO_(2) emissions.However,when rock powder was added to the seawater-CO_(2) mixture,the pH increased.This suggests that the EW of ultramafi c rock powders can sequester CO_(2) while raising seawater pH through the formation of secondary minerals.This research could serve as an analog for EW applications,considering the worldwide abundance of ultramafi c rocks and the availability of coastal and open ocean environments.However,further research is required to understand the behavior of other elements and their impacts on ocean chemistry in EW processes before applying CO_(2) sequestration strategies.
文摘The site of Mansehra is located seismically in an active regime, known as the Crystalline Nappe Zone and Hazara-Kashmir Syntaxis in NW Himalayas, Pakistan. Seismic Hazard Assessment （SHA） for the site has been carried out by considering the earthquake source zones, selection of appropriate attenuation equations, near fault effects and maximum potential magnitude estimation. The Mansehra Thrust, Oghi Fault, Banna Thrust, Balakot Shear Zone, Main Boundary Thrust, Panjal Thrust, Jhelum Fault and Muzaffarabad Fault and, further to the south, the Sanghargali, Nathiagali, and Thandiani Thrusts are the most critical tectonic features within the 50 km radius of Mansehra. Using the available instrumental seismological data from 1904 to 2007, SHA has been carried out. Other reactivated critical tectonic features in the area have been investigated. Among them the Balakot-Bagh fault, with the fault length of 120 km from Balakot to Poonch, has been considered as the most critical tectonic feature on the basis of geological/structural/seismological data. The potential earthquake of maximum magnitude 7.8 has been assigned to the Balakot-Bagh fault using four regression relations. The peak ground acceleration value of 0.25 g （10% probability of exceedance for 50 years） and 0.5 g has been calculated with the help of the attenuation equation using probabilistic and deterministic approaches.
文摘An attempt has been made to systematically revise the Late Cretaceous （Turonian） bivalves of the Bagh Beds, central India. Altogether, fifteen species have been described here. The two species Nicaniella （N） trigonoides ＆ Protocardia （P） laticostata, which are earlier known from Late Cretaceous of Tiruchirapalli subbasin, southern India, have been recorded for the first time from Narmada Basin. The other species recorded are： Modiolus typicus, Neithea morrisi, Plicatula batnensis, P. numidica, P. instabilis, Lucina （L.） cf. fallax, Astarte similis, Opis corniformis, Protocardia hillana, P. madagascariense, Cytherea （Callista） lancianata, Trigonocallista spathi and Pholadomya sp.. During course of systematic revision, it has been found that many species described by earlier workers from the Late Cretaceous of Bagh Beds have been found conspecific to already known species from the Cretaceous of different parts of the globe and hence, they have been recorded here as junior synonyms. These species have immense implication in the palaeobiogeography of the region.
基金Authors are thankful to the Ministry of Earth Sciences,Government of India,for financial support in the form of Extra-Mural Research Project(Ref.No.Mo ES/P.O.(Geo)/142/2017)。
文摘Rising sea-levels in tectonically active epicontinental basins often lead to varied depositional settings and palaeogeography, mostly influenced by the net accommodation resulting from mutual interference of the extent and nature of landward encroachment by the sea and the net sedimentation. The Cenomanian Nimar Sandstone Formation, Bagh Group, Narmada rift basin, uniquely portrays the effect of sea-level rise within an intra-cratonic setting and attributes to the corresponding palaeogeographic changes in west-central India. An integrated sedimentological–sequence-stratigraphic study of the broadly fining-upward Nimar Sandstone Formation(thickness~ 20–30 m) depicts the actual nature of changeover from a fluvial to a marine-dominated transitional depositional setting. Detailed sedimentological study reveals total seventeen facies, grouped in five facies associations, viz., the channel-fill facies association(FA-1), the overbank facies association(FA-2), the fluvial-dominated fluvio-tidal facies association(FA-3), the tide-dominated fluvio-tidal facies association(FA-4), and the shoreface facies association(FA-5). Overall facies architecture indicates a west-to-eastward marine encroachment, resulting in stacking of three distinct palaeo-depositional conditions:(i) an initial fluvial system with channel and overbank, changing into a tideinfluenced fluvial bay-head delta in the inner estuary, followed by(ii) marine encroachment leading to a tidedominated central estuary with inter-to sub-tidal settings, and finally,(iii) with further intense marine encroachments, a wave-reworked open shore condition in the outer estuary zone. The overall fining-up succession with a systematic change from fluvial to marine-dominated depositional systems points to a landward shift of the shoreline, signifying a major transgressive event correlated to the Cenomanian global sea-level rise. Characteristic stratal stacking patterns point to four coarsening-and fining-up hemicycles, embedded within the major transgressive succession. These high-frequency cycles attest to the varied interplay of sedimentation, tectonics and sea-level changes, and the resultant net accommodations. A palaeogeographic model is proposed based on the high-frequency transgressive–regressive hemicycles, which envisages the evolution of the depositional environments in relation to the Cenomanian eustatic rise in the intra-cratonic riftogenic fluvio-marine transitional basinal setup.
