The document summarizes the stratigraphy of the Mesozoic sedimentary basins of Kutch and Cretaceous sedimentary succession in Ariyalur district, India. It describes the depositional environments, lithology, thickness, and fossil content of the different formations in these basins. The Kutch basin formed due to rifting in the Mesozoic and contains over 3000m of sediments ranging from Triassic to Cretaceous in age. The Cretaceous succession in Ariyalur district represents a marine transgression and contains rich fossil records across formations totaling over 2300m of sediments deposited over 35 million years.
The term "trap" has been used in geology since 1785–95 for rock formations. It is derived from the Swedish word for stairs (trapp , trappa) and refers to the step-like hills forming the landscape of the region.
The plateau: also called a high plain or tableland, is an area of highland, usually consisting of relatively flat terrain. A plateau is an elevated land. It is a flat-topped table standing above the surrounding area. A plateau may have one or more sides with steep slopes.
LIP – Large Igneous provinces. (Province = Area / Region)
DVP - The Deccan Volcanic Province is one of the Earth’s giant continental flood basalts and has a total exposed area of about half a million square kilometers in Maharashtra, Madhya Pradesh, Gujrat and some part of Andhra Pradesh. Deccan trap has maximum thickness 3400m in western ghat and its thickness goes decrease toward east side. At Amrakantat on east its thickness is just 160m. Geographical distribution is between latitudes 16° - 24° N and longitudes 70° - 77° E.
The term "trap" has been used in geology since 1785–95 for rock formations. It is derived from the Swedish word for stairs (trapp , trappa) and refers to the step-like hills forming the landscape of the region.
The plateau: also called a high plain or tableland, is an area of highland, usually consisting of relatively flat terrain. A plateau is an elevated land. It is a flat-topped table standing above the surrounding area. A plateau may have one or more sides with steep slopes.
LIP – Large Igneous provinces. (Province = Area / Region)
DVP - The Deccan Volcanic Province is one of the Earth’s giant continental flood basalts and has a total exposed area of about half a million square kilometers in Maharashtra, Madhya Pradesh, Gujrat and some part of Andhra Pradesh. Deccan trap has maximum thickness 3400m in western ghat and its thickness goes decrease toward east side. At Amrakantat on east its thickness is just 160m. Geographical distribution is between latitudes 16° - 24° N and longitudes 70° - 77° E.
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Kutch is an East-west Oriented pericraton Rift basin Situated between Nagar Parkar Fault in North and Kathiawar Uplift in South.
Here we will discuss Geology and its Sequence Stratigraphy.
Kutch Basin Sequence Stratigraphy.
Kutch is an east-west oriented pericratonic basin comprising of rocks ranging from Mesozoic to Cenozoic.
Kutch Basin experienced various phases of marine Transgression and Regression throughout its Geological History.
for More Information email at ravgou39@gmail.com
Karai badland topography and Geo-Heritage site, Take A Geotourism around Grav...sutikshandwivedi
The Karai Badlands national geological monument is located in the Karai area along the Karai-Kulakkalnattam road of Perambalur District, Tamil Nadu. A four km. the stretch of badlands with natural conical mounds and typical fossils of the Cretaceous age is exposed as badlands with a series of conical mounds separated by gulleys.
Badland topography, on either side of Alattur-Ariyalur road, spread within 40-70 km. radius marks the lower part of marine Cretaceous rocks that mainly consists of clay & sandstone of the Karai Formation. Like the Grand Canyon in Colorado, US, Ariyalur is considered a Cretaceous Park of South India by Geo-scientist.
The Geological Survey of India (GSI), has declared Karai Badland as a National Geological monument for its maintenance, protection, promotion, and enhancement of geo-tourism.
Stratigraphy
The Rock formation is here exposed to the Cretaceous of Trichinopoly, Which dates back to the Late Cretaceous. The Succession in the area is broadly divided into 4 Groups -Uttathur, Trichinopoly, Ariyalur, and Ninniyur, Where Uttathur is the oldest. After comparing the age and color of the rock formations here with those of the Himalayas, we have found that they are of the same age. The Karai Formation of Uttatur Group at the Karai-Kulakkalnattam section in the Perambalur district forms the lower part of the Cretaceous sedimentary succession of the Cauvery Basin.
The Karai Badlands area is the type area for Karai Formation. The Karai Formation is exposed as badlands with a series of conical mounds separated by gulleys. It is a wasteland with scanty vegetation and without any topsoil on either side of Karai-Kulakkalnattam road.
The Karai Badlands Formation consists of grey-brown, gypsiferous, glauconitic mudstone, and marl with sporadic thin interbeds of siltstone and calcareous sandstone, particularly in its upper part- sporadic calcareous, siderites and phosphatic concretions/nodules and concretionary horizons occur in some intervals. A variety of marine fossils like ammonites, nautiloids, belemnites, worm tubes, pelecypods, gastropods, and oysters occur in abundance.
The importance of this “Geoheritage Site” lies in the fact that it provides one of the best-exposed sections of Cretaceous rocks with its unique lithology and diversity of extinct marine life. The region is a magnet for cement companies because of the purity of Ariyalur’s limestone. The factories burn a mixture of powdered limestone, gypsum, coal, and other chemicals to produce cement and clinker. But unchecked mining has led to air pollution and large quantities of overburdened soil being heaped up randomly.
How Badland is a form
The Cretaceous Period (135- 65 Million Years) witnessed a series of major geological events in the history of the Earth. Of these, the most significant is the worldwide marine transgression, which has left its mark in many parts of the world including South India.
·
archaeocyathid
o
Cambrian - sessile, reef-building marine organisms of warm tropical and subtropical waters that lived during the early (lower) Cambrian period.
·
bioturbation
o
Cambrian - the reworking of soils and sediments by animals or plants. Its effects include changing texture of sediments (diagenetic), bioirrigation and displacement of microorganisms and non-living particles. Common bioturbators include annelids and bivalves (mussels, clams, gastropods).
·
Burgess Shale
o
Cambrian - located in the Canadian Rockies of British Columbia, is one of the world's most celebrated fossil fields. It is famous for the exceptional preservation of the soft parts of its fossils. At 505 million years (Middle Cambrian) old, it is one of the earliest fossil beds containing soft-part imprints.
·
Cambrian explosion
o
Cambrian - the relatively rapid appearance, around 530 million years ago, of most major animal phyla, as demonstrated in the fossil record, accompanied by major diversification of organisms
·
Iapetus Ocean
Cambrian/Ordovician - Precursor to the Atlantic. An ocean that existed in the Neoproterozoic and Paleozoic eras of the geologic timescale (between 600 and 400 million years ago). The ocean disappeared with the Caledonian, Taconic and Acadian orogenies, when these three continents joined to form one big landmass called Laurussia.
maturity Cambrian
·
Paleozoic Era
o
Cambrian - the earliest of three geologic eras of the Phanerozoic Eon, spanning from roughly 541 to 252.2 million years ago. It is the longest of the Phanerozoic eras, and is subdivided into six geologic periods (from oldest to youngest): the Cambrian, Ordovician, Silurian, Devonian, Carboniferous, and Permian.
·
passive margin
o
Cambrian - the transition between oceanic and continental crust which is not an active plate margin. It is constructed by sedimentation above an ancient rift, now marked by transitional crust. Continental rifting creates new ocean basins.
·
trilobite
o
Cambrian - extinct marine arthropods that form the class Trilobita. Trilobites form one of the earliest known groups of arthropods. Trilobites finally disappeared in the mass extinction at the end of the Permian about 250 million years ago. The trilobites were among the most successful of all early animals, roaming the oceans for over 270 million years.
·
bentonites
o
Ordovician - essentially impure clay consisting mostly of montmorillonite. Bentonite usually forms from weathering of volcanic ash, most often in the presence of water. However, the term bentonite, as well as a similar clay called tonstein, has been used to describe clay beds of uncertain origin.
·
Cincinnati arch
o
Ordovician - when continents crashed together during the two orogeny's you have the Appalachian mountains and then a down drop into the Appalachian basin going west and then going west the next rise is the Cincinnati arch and the next basin is the Illinois basin.
epeir.
Connector Corner: Automate dynamic content and events by pushing a buttonDianaGray10
Here is something new! In our next Connector Corner webinar, we will demonstrate how you can use a single workflow to:
Create a campaign using Mailchimp with merge tags/fields
Send an interactive Slack channel message (using buttons)
Have the message received by managers and peers along with a test email for review
But there’s more:
In a second workflow supporting the same use case, you’ll see:
Your campaign sent to target colleagues for approval
If the “Approve” button is clicked, a Jira/Zendesk ticket is created for the marketing design team
But—if the “Reject” button is pushed, colleagues will be alerted via Slack message
Join us to learn more about this new, human-in-the-loop capability, brought to you by Integration Service connectors.
And...
Speakers:
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Charlie Greenberg, Host
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Session Overview
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During this webinar, we will cover the following topics while demonstrating the integrations of JMeter, InfluxDB and Grafana:
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Dev Dives: Train smarter, not harder – active learning and UiPath LLMs for do...UiPathCommunity
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Get an exclusive demo of the new family of UiPath LLMs – GenAI models specialized for processing different types of documents and messages
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LF Energy Webinar: Electrical Grid Modelling and Simulation Through PowSyBl -...DanBrown980551
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PowSyBl is an open source project hosted by LF Energy, which offers a comprehensive set of features for electrical grid modelling and simulation. Among other advanced features, PowSyBl provides:
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2.
Among the different basins in the western sector, the Mesozoic basins of
Kutch and Jaisalmer range from Triassic well into the Upper Cretaceous with
some break in the sedimentation. These enclose sediments of 1500-3000 m
thickness in Kutch and about 800 m in Jaisalmer, covering 43000 sq. km
including about 15000 sq. km and 800 sq. km respectively of exposed
sedimentary areas.
The basins of Kutch and Jaisalmer owe their formation to rifting along the
major Precambrian lineaments in Western India- East Africa divergent plate
region, prior to the fragmentation of Gondwana superplate.
The successions in both these basins are thick, well developed and organically
rich, exhibiting a fair degree of stratigraphic simiarity. The sediments, except
for the Middle Jurassic carbonates, are dominantly siliciclastic. A marine
facies is advocated for the successions, including the plant- fossil bearing part
of the succession, traditionally held to be non-marine.
3.
Mesozoic rocks ranging in age from Middle Jurassic to lower Cretaceous are
exposed in the following six disconnected areas: (i) Kutch Mainland
(ii)Patcham “Island”(iii) Khadir “Island”(iv) Bela “Island” (v) Chorar “Island”
(vi) Wagad
Wynne mapped Mesozoic rocks of Kutch. Stoliczka and Waagen studied the
fossils and it is the latter who suggested the well known subdivisions of
Patcham ,Chari ,Katrol and Umia in the ascending order.
4.
Mesozoic sedimentation in Kutch basin, in general, commenced with the
deposition of retrogradational and aggradational succession (RS & AS) in the
lower part followed by the progradational succession(PS)in the upper part.
About 200 m of Aalenian sediments are nonmarine and transgression starts
with. RS and AS deposited during Aalenian-Tithonian, exibit overlapping,
thick highly fossiliferous limestone/sandstones. PS deposited during
Neocomian (?)- Turonian – Coniacian represents sandy lithologies of
coarsening upward, offlapping sandstones, shales and thin limestones.
Qualitative and quantitative analyses of heavy minerals, quartz grains and
lithic fragments suggest at least two lithologically different Precambrian
provenances, during Mesozoic, namely (i) the Aravalli Range of Rajasthan
towards north and east and (ii) the Nagar- Parkar massif (granites, syenites)
toward north and northwest, partly in Pakistan.
5.
STRATIGRAPHY:
The Umia Formation is diffrentiated into members in northwest Kutch only,
but elsewhere in the mainland, it is undiffentiated above Katrol Formation.
The Dhosa Oolite Member occurs at the top of the Chari Formation all over
Kutch Mainland.
Patcham Formation is present only in Patcham “island” and Jumara Dome.
6.
The western margin of Indian Peninsular Shield is affected by rifting along major
Proterozoic orogenic trends viz., Aravalli-Delhi and Satpura mobile belts. Kutch
rift is the northern most pericontinental embayed basin situated between the
subsurface Nagar Parkar Uplift(NPU) in the north, Radhanpur- Barmer arch in the
east and Kathiawar Uplift in the south. The two uplifts are the rift shoulders
respectively along Nagar Parkar Fault(NPF) and North Kathiawar Fault(NKF) and
the Radhanpur- Barmer arch is the rift and hinterland. This arch is the western
shoulder of the Cambay rift, which terminates the west to east Kutch rift. Besides
horsts(H), grabens (G) and half- grabens(HG), there are anticlines and domes of
varying sizes and shapes.
The Kutch basin evolved in two stages : (i) Rift stage: basin subsidence along
faults and (ii) Inverse stage: uplifts along the same faults by reverse movements.
The east-west oriented, fault bounded, ridges and depressions influnced the
thickness and facies distribution of the formation here. The westerly plunge of the
basin is reflected in the general westward thickening of the sedimentary units
deposited during the two Mesozoic transgressive and regressive cycles,and their
relatively deeper- shelf facies prograding towards west.
7.
The rich ammonoid faunas of Kutch Jurassic together with those of the
Tethys Himalaya have a significant bearing on the nature and the extent
of the faunal provinces within the Tethyan realm as also on the marine
seaways connecting them. Biogeographical reconstruction made with the
available data invariably present a direct and often persistent marine
connection at least from late Early Jurassic onwards from East Africa,
Madagascar, Kutch, Jaisalmer, Salt Range, Spiti, Nepal, south Tibet and
also to Sula Islands to New Guinea.
The Callovian stage in Kutch is onsidered to be the one best developed in
the world, while Kutch Jurassic sequence as a whole is considered of
primary reference in the entire East Tethyan region.
Earliest known occurances of nannofossils, the tiniest (1- 30 microns)
marine calcareous microfossils, are from Early Jurassic. The broad groups
that are included in the study of nannofossils are the extant
Coccolithophorids and the extinct discoasters and nannoconids.
Nannoflora of the Chari Formation has proven to be the best known in
the world.
8.
The great Cenomanian (98 Ma) transgression covered considerable area in
the soth eastern part of Tamil Nadu between the Cauvery river and
Pondicherry. Ponniar and Vellar rivers separate the areal distribution into
three disconnected regions, viz. Pondicherry, Vridhachalam and
Ariyalur(eastern part of Trichinopoly district). Of these, the outcrops near
Trichinopoly are the largest with an areal extent of about 400 sq. km
ranging in age from Aptian/ Albian to early Paleocene with a
stratigraphic record of nearly 120- 61 Ma. The edimentation is often
interrupted by low angle unconformities.
9.
The Archean crystalline gneisses and charnokites with a NE-SW trend
constitute the floor for this depocentre. Small hillocks along the
Perambalur- Trichinopoly road delimit the western margin. The Boulder
Conglomerate is a classic example for fanglomerate, derived from a
tectonicaly active source due to faulting, in association with coalescing
alluvial fans. The Terani Plant Beds, a unit of kaolinitic clay and
ferruginous sand interbeds, are well known for their rich plant fossils. A
low energy inland lacustrine environment is ascribed to this unit.
The Cretaceous sediments dip at very low angles, though higher dis have
been recorded close to the contact zones of the sediments with the
cystalline rocks. The sediments of the Uttatur and Trichinopoly Groups
show evidences of folding. The faults traced at the western boundary of
the Cretaceous sediments are thought to be reactivated Precambrian
faults.
10.
An attempt has been made to infer sedimentation rate, relative sea levels and
transgression cycles in the Cretaceous succession in the Ariyalur district based
on the study of 2325 m mid- Cretaceous –Paleocene sequence, over an
interval of about 35 Ma. The mean rate of sedimentation is estimated to have
varied between 15 and 240 mm per thousand years.
Uttatur Group: Basal conglomerate, grey shales , sponge- coral- algal
limestone and shale/ clay distinguish this group, resting unconformably over
the basement with phosphatic nodules having a maximum thickness of about
600 m.
The Grey Shale, occuring below the Kallakudi Limestone, appears to be
extensive unit and it has been logged in the subsurface in different parts of
Cauvery basin and identified as primary source of generating hydrocarbons.
The Kallakudi/(Dalmiapuram) Limestone, which is actively mined for
cement, is a sponge coral- algal reefal limstone. the age of this unit is Middle
Aptian- Middle Albian. The limestone is presumably deposited in an
intertidal zone in a protected still- water bay.
11.
Trichinopoly Group: The group unconformably rests over the Uttatur,
and it is well evident at places. It is divisible into lower Kulakkalnattam
and upper Anaipadi Formations separate from each other by a
conglomerate bed. Kulakkalnattam Formation is a calcareous sandstone
unit with ferruginous concretionary bodies extensively bioturbated by
feeding burrows like Thalassinoides. It is intercalated with dark grey
limestone containing thick- shelled bivalves (Oysters), ammonites,
rhynconellids, brachiopods and silicified wood. The thickness of the unit
is about 60 m.
The succeeding unconformably overlying Anaipadi Formation is
essentially made of sandstones, siltstones with concretionary layers rich
in fossils.the thickness of this group is about 100 m. A regressive near
coastal environment is suggested for the sedimentation of this group.
12.
Ariyalur Group: It lies unconformably over the Trichinopoly Group and
consists of two dominantly sadstones bodies seperated by limestones. The
lower Sillakudi Formation comprises ferruginised arkosic sandstones and
limestone bands. The depositional environment appears to be high- energy
transgressive tidal bars or shoals.
The Kallankurichi Formational, resting unconformably over the Sillakudi
Formation, is a massive rudist bivalve carbonate shell- bank of about 40 m
thickness. This carbonate unit is considered to be a shallow marine carbonate
bank/ shoal deposit.
The overlying calcareous sandstone, of about 60 m thickness, mapped as
Ottakovil Formation . The age is Maastrichtian. The lithology and faunal
remains are suggestive of marginal marine to near shore condition of
deposition.
It is overlain by white to grey, cross- bedded thick sandstones intercalated
with greenish grey to red clays, which delimit the Cretaceous succession
known as Kallamedu Formation in which the presence of reptilian fossils such
as bones of Megalosaurus, Titanosaurus have been reported.
13.
Ninyur Formation : The Cretaceous succession is unconformably overlain
by a thick carbonate sequence is of about 60 m in thickness. Lithologically
this unit is divisible into lower fossiliferous limestone, middle
recrystalline shelly limestone and upper argillaceous gritty nodular
limestone collectively known as Ninyur Formation. These carbonate beds
are too mined for cement industry.